Analysis of pore-fracture structure evolution and permeability in tar-rich coal under high-temperature pyrolysis using μCT technology

热解 磁导率 开裂 多孔性 材料科学 tar(计算) 煤焦油 复合材料 化学工程 矿物学 地质学 化学 有机化学 生物化学 计算机科学 工程类 程序设计语言
作者
Pengfei Jiang,Zhongyan Cheng,Jia‐Qi Huang,Gaigai Li
出处
期刊:Geomechanics and geophysics for geo-energy and geo-resources [Springer Science+Business Media]
卷期号:10 (1)
标识
DOI:10.1007/s40948-024-00826-1
摘要

Abstract To study the internal evolution characteristics of tar-rich coal under high-temperature pyrolysis and improve pyrolysis efficiency, three-dimensional reconstruction and analysis of tar-rich coal from northern Shaanxi after high-temperature pyrolysis were conducted using μCT technology. The evolutionary development of pore and fracture structure at different temperatures and the relationship between pore-fractures and permeability was studied and discussed. The results show that when tar-rich coal from 300 to 600 °C, it mainly undergoes two stages: in the first stage, the internal substance structure of the coal mainly undergoes thermal cracking, forming large fracture bands; in the second stage, the coal undergoes intense pyrolysis reactions, resulting in primarily circular or elliptical large pore structures within the coal, with a reduction in the number of fractures. Furthermore, a strong exponential relationship is exhibited between the porosity and permeability of tar-rich coal, and a predictive equation is provided. When the temperature exceeds 500 °C, the coupled effect of pores and fractures contributes more than 20% to permeability, and its impact cannot be ignored.
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