2018
DOI: 10.3390/su10103587
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Changes in the Distribution of Temperature in a Coal Deposit and the Composition of Gases Emitted during Its Heating and Cooling

Abstract: This article presents the results of tests conducted on a measuring system for monitoring changes in the distribution of temperature in a coal deposit during the heating and cooling phases, and their correlation with the analysis of the concentration of gases. The tests were conducted on five samples of hard coal collected in deposits mined in Poland. Measurements of the changes in temperature and changes in gas concentration were conducted from the temperature of 35 to 300 °C, for the heating phase, and from … Show more

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Cited by 6 publications
(4 citation statements)
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“…In this process, coal and other carbonaceous materials self-heat thereby resulting in ignition known as spontaneous heating. When coal is given enough oxygen, it can spontaneously heat up, and the coal can store the heat that is released (Więckowski, Howaniec, Postnikov, Chorążewski, & Smoliński, 2018).…”
Section: Spontaneous Combustionmentioning
confidence: 99%
“…In this process, coal and other carbonaceous materials self-heat thereby resulting in ignition known as spontaneous heating. When coal is given enough oxygen, it can spontaneously heat up, and the coal can store the heat that is released (Więckowski, Howaniec, Postnikov, Chorążewski, & Smoliński, 2018).…”
Section: Spontaneous Combustionmentioning
confidence: 99%
“…The phenomena of coal self-heating are accompanied by numerous processes hindering the appropriate assessment of fire hazard, including the natural desorption of gases from coal 7 , 8 . The main gas emitted during the process of low temperature self-heating of coal is methane, while carbon monoxide was proven and implemented as the main indicator of the development of low temperature self-ignition of coal 9 .…”
Section: Introductionmentioning
confidence: 99%
“…This phenomenon is connected with the process of permeability changes within the ECBM technology [7]. The transformation of pore and cleat structures of coal connected with the supercritical CO 2 leads to the increase in permeability within the zone of coal strata, which constitutes a key factor for CO 2 sequestration and the efficiency of CH 4 production [8][9][10]. Lowering the pressure of fluids in the production well and the removal of coal seam waters, which initiates the process of methane desorption accelerated by injecting CO 2 to the coal seam through the injection well, constitute the point of departure.…”
Section: Introductionmentioning
confidence: 99%