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Frontiers in Energy

ISSN 2095-1701

ISSN 2095-1698(Online)

CN 11-6017/TK

Postal Subscription Code 80-972

2018 Impact Factor: 1.701

Front. Energy    2021, Vol. 15 Issue (2) : 320-327    https://doi.org/10.1007/s11708-020-0674-3
RESEARCH ARTICLE
Effective diffusivity of oxygen in the ash layer of Huadian oil shale semicoke
Yiqun HUANG1, Yiran LI1, Man ZHANG1, Boyu DENG1, Hao KONG1, Junfeng WANG2, Junfu LYU1, Hairui YANG1(), Lingmei WANG3()
1. Key Laboratory for Thermal Science and Power Engineering of the Ministry of Education, State Key Laboratory of Power Systems, Department of Energy and Power Engineering, Tsinghua University, Beijing 100084, China
2. State Key Laboratory of Efficient and Clean Coal-fired Utility Boilers (Harbin Boiler Co., Ltd.), Harbin 150046, China
3. Department of Automation, Shanxi University, Taiyuan 030006, China
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Abstract

Diffusion of oxygen in the ash layer usually dominated the combustion of oil shale semicoke particles due to the high ash content. Thus, effective diffusivity of oxygen in the ash layer was a crucial parameter worthy of careful investigation. In this paper, the effective diffusivity of oxygen in the ash layer of Huadian oil shale semicoke was measured directly using an improved Wicke-Kallenbach diffusion apparatus. The experimental results showed that higher temperature would lead to a higher effective diffusivity and a thicker ash layer had the negative effect. Especially, the effective diffusivity along the direction perpendicular to bedding planes was much lower than that along the direction parallel to bedding planes. In addition, an effective diffusivity model was developed, which could be used to describe the mass transfer of oxygen in the ash layer of oil shale semicoke.

Keywords oil shale semicoke      diffusivity      pore structure      ash layer     
Corresponding Author(s): Hairui YANG,Lingmei WANG   
Online First Date: 11 June 2020    Issue Date: 18 June 2021
 Cite this article:   
Yiqun HUANG,Yiran LI,Man ZHANG, et al. Effective diffusivity of oxygen in the ash layer of Huadian oil shale semicoke[J]. Front. Energy, 2021, 15(2): 320-327.
 URL:  
https://academic.hep.com.cn/fie/EN/10.1007/s11708-020-0674-3
https://academic.hep.com.cn/fie/EN/Y2021/V15/I2/320
Fig.1  Wicke-Kallenbach diffusion apparatus.
Fig.2  Experimental results of four different gas admission rates (at an ash thickness of 5 mm and a diffusion temperature of 293 K).
Mar Aar Var FCar Qar,net/(kJ·kg–1) C H N S
1.11 77.73 12.98 8.18 4767.2 13.55 0.31 0.22 1.12
Tab.1  Proximate analysis, ultimate analysis, and heat value of Huadian oil shale
Fig.3  Schematic of samples in the direction parallel and perpendicular to bedding planes.
Fig.4  Effective diffusivities in the direction parallel to bedding planes at different gradients of oxygen concentration (at an ash thickness of 10 mm).
Fig.5  Effective diffusivities in the direction parallel to bedding planes at different diffusion temperatures.
Fig.6  Effective diffusivities in the direction parallel to bedding planes at different ash layer thicknesses.
Fig.7  Pore size distributions of ash layers at different thicknesses.
Fig.8  Schematic of oxygen diffusion in ash layer.
Fig.9  Comparison of effective diffusivity in the direction parallel and perpendicular to bedding planes (at a diffusion temperature of 293 K and an ash layer thickness of0.005 m).
Fig.10  SEM photography of ash layer plane.
Fig.11  A diffusion example with two diffusivities.
Fig.12  Experimental results versus model results.
Fig.13  Effective diffusivity of the whole ash layer versus diffusivity at the infinitesimal element (at a diffusion temperature of 1073 K)
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