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Numerical modelling of unsteady transport and entropy generation in oxy-combustion of single coal particles with varying flow velocities and oxygen concentrations

Numerical modelling of unsteady transport and entropy generation in oxy-combustion of single coal particles with varying flow velocities and oxygen concentrations
Numerical modelling of unsteady transport and entropy generation in oxy-combustion of single coal particles with varying flow velocities and oxygen concentrations
Unsteady generation of entropy and transfer of heat and chemical species in the transient oxy-combustion of a single coal particle are investigated numerically. The burning process takes place in oxygen and nitrogen atmospheres with varying chemical compositions and under either quiescent or active flows. The combustion simulations are validated against the existing experimental data on a single coal particle burning in a drop-tube reactor. The spatio-temporal evolutions of the gas-phase temperature and major gaseous species concentration fields as well as that of entropy generation are investigated for the two types of gas flow. It is shown that the rates of production and transport of chemical species reach their maximum level during the homogenous combustion of volatiles and decay subsequently. Yet, the transient transfer of heat of combustion continues for a relatively long time after the termination of particle life time. This results in the generation of a large amount of thermal entropy at post-combustion stage. The analyses further indicate that the entropy generated by the chemical reactions is the most significant source of unsteady irreversibilities. Most importantly, it is demonstrated that a slight oxygenation of the atmosphere leads to major increases in the total chemical entropy generation and, thus it significantly intensifies the global irreversibilities of the process. However, upon exceeding a certain mole fraction of oxygen in the atmosphere, further addition of oxygen only causes minor increases in entropy generation. This trend is observed consistently in both quiescent and active flow cases.
1359-4311
147-164
Wang, L.
6776fc93-419c-493c-9964-d2ec21e4b598
Karimi, N.
620646d6-27c9-4e1e-948f-f23e4a1e773a
Sutardi, T.
aceaae0c-153a-4649-a9ca-10c71d0ef8a2
Paul, M.C.
260ddeb9-6eed-4495-a8e0-2ebd2dc88917
Wang, L.
6776fc93-419c-493c-9964-d2ec21e4b598
Karimi, N.
620646d6-27c9-4e1e-948f-f23e4a1e773a
Sutardi, T.
aceaae0c-153a-4649-a9ca-10c71d0ef8a2
Paul, M.C.
260ddeb9-6eed-4495-a8e0-2ebd2dc88917

Wang, L., Karimi, N., Sutardi, T. and Paul, M.C. (2018) Numerical modelling of unsteady transport and entropy generation in oxy-combustion of single coal particles with varying flow velocities and oxygen concentrations. Applied Thermal Engineering, 144, 147-164. (doi:10.1016/j.applthermaleng.2018.08.040).

Record type: Article

Abstract

Unsteady generation of entropy and transfer of heat and chemical species in the transient oxy-combustion of a single coal particle are investigated numerically. The burning process takes place in oxygen and nitrogen atmospheres with varying chemical compositions and under either quiescent or active flows. The combustion simulations are validated against the existing experimental data on a single coal particle burning in a drop-tube reactor. The spatio-temporal evolutions of the gas-phase temperature and major gaseous species concentration fields as well as that of entropy generation are investigated for the two types of gas flow. It is shown that the rates of production and transport of chemical species reach their maximum level during the homogenous combustion of volatiles and decay subsequently. Yet, the transient transfer of heat of combustion continues for a relatively long time after the termination of particle life time. This results in the generation of a large amount of thermal entropy at post-combustion stage. The analyses further indicate that the entropy generated by the chemical reactions is the most significant source of unsteady irreversibilities. Most importantly, it is demonstrated that a slight oxygenation of the atmosphere leads to major increases in the total chemical entropy generation and, thus it significantly intensifies the global irreversibilities of the process. However, upon exceeding a certain mole fraction of oxygen in the atmosphere, further addition of oxygen only causes minor increases in entropy generation. This trend is observed consistently in both quiescent and active flow cases.

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Published date: 5 November 2018

Identifiers

Local EPrints ID: 508908
URI: http://eprints.soton.ac.uk/id/eprint/508908
ISSN: 1359-4311
PURE UUID: 2ed9cae0-3e39-49bb-a3c9-b767bae16830
ORCID for N. Karimi: ORCID iD orcid.org/0000-0002-4559-6245

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Date deposited: 05 Feb 2026 17:55
Last modified: 06 Feb 2026 03:12

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Contributors

Author: L. Wang
Author: N. Karimi ORCID iD
Author: T. Sutardi
Author: M.C. Paul

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