4.7 Article

Radon exhalation characteristics after pyrolysis of long flame coal

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 904, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.scitotenv.2023.167228

关键词

Mining area; High temperature; Coal pyrolysis; Radon exhalation; Pore structure; Environmental pollution

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Coal pyrolysis is an important method for utilizing coal resources, but it may release radioactive gas radon during high-temperature pyrolysis. This study conducted experiments to measure the radon release concentration of pyrolysis products in different atmospheric environments and found a negative correlation between the heat treatment temperature and the radon release rate.
Coal pyrolysis is a important method for classifying and utilizing coal resources and contributes to enhanced comprehensive resource utilization. However, In high-temperature areas such as coal pyrolysis, there is an abnormal phenomenon release of radioactive gas radon, understanding the relationship between temperature and radon exhalation characteristics, as well as the underlying mechanisms, holds great importance for assessing radon pollution in mining areas. After coal undergoes pyrolysis under high temperature conditions, its material composition, pore structure, water content, and other properties have changed. The pyrolysis products in different atmosphere environments have differences, and the characteristics of radon emission are also different. To address this, the present study conducted coal pyrolysis experiments in both aerobic and anaerobic environments, using long flame coal sourced from Yulin, China. The radon release concentration of the pyrolysis products was measured. The research findings indicate that during pyrolysis at elevated temperatures, the ratio of coal mass loss is constantly increasing. High temperatures promote the development of pores and fissures, and significant changes in coal properties at temperature thresholds (300 C-degrees and 500 C-degrees). The specific surface area, pore volume, and fracture ratio all display substantial increases, and the amplitude of change is greater under aerobic conditions. The fractal dimension of total pores and macropores shows continuous growth, while the specific surface area, pore volume, and fracture ratio exhibit a strong negative correlation with the radon emission rate of pyrolysis products. The expansion and penetration of pores and cracks, along with the release of a substantial amount of pyrolysis gas, accelerate the transformation, migration, and exhalation of radon, resulting in a negative correlation between the heat treatment temperature and the radon release rate of pyrolysis products. Under aerobic conditions, the radon release rate of pyrolysis products decreases more significantly.

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