4.6 Article

Experimental Investigation on the Pore Structure Evolution of Coal in Underground Coal Gasification Process

Journal

ACS OMEGA
Volume 7, Issue 13, Pages 11252-11263

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acsomega.2c00157

Keywords

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Funding

  1. Beijing Natural Science Foundation [3212020]
  2. National Natural Science Foundation of China [52004303]
  3. Science Foundation of the China University of Petroleum, Beijing [2462020YXZZ032]

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This study investigated the evolution of pore structure during the heating process of coal. The results showed that the heating process can be divided into three stages, dominated by drying, primary pyrolysis, and secondary pyrolysis reactions at different temperature ranges. The coal transformed into porous char or ash framework during the heating process.
Underground coal gasification (UCG) has been shown to be a promising method for deep coal resources. A series of complicated chemical reactions can induce a considerable change in the pore structure of coal and thus promote the UCG process in turn. Currently, most studies on the effect of elevated temperature on the pore structure of coal were not involved in an air atmosphere, bringing a series of difficulties to understanding the pore structure evolution of gasified coal in the UCG process. The objective of this work was to investigate the pore structure evolution of coal heated in nitrogen and air atmospheres at elevated temperatures. Thermogravimetry tests were first conducted to gasify coal samples, and then, the method scanning electron microscopy was used to observe the microscopic morphology of the pore structure. Besides, the effect of final temperature, atmosphere, pressure, and residence time on the thermal dynamics of coal at elevated temperatures was comprehensively discussed. Results indicated that the temperature range of a heating process of coal can be classified into three stages, 25-320 degrees C, 320-750 degrees C, and 750-1000 degrees C. For the three temperature ranges, drying, primary pyrolysis, and secondary pyrolysis can dominate, respectively, under a nitrogen atmosphere, while the combustion and gasification process will prevail at a high temperature under an air atmosphere. Because of mass loss, the coal was becoming porous during the heating process. Compared with the intact structure of coal when the temperature is lower than 300 degrees C, the pore space can interconnect under moderate-temperature conditions (500 degrees C) like a honeycomb, and then, only an ash framework remained under a higher-temperature condition (700 degrees C) under an air atmosphere. In comparison, the coal heated in a nitrogen atmosphere can gradually turn into a porous char. This investigation can provide some new insights into the pore structure evolution of gasified coal and contribute to the mechanisms of a UCG process.

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