THERMOGRAVIMETRIC EXPERIMENTAL STUDIES OF THE EXPLOSION HAZARD OF COAL DUST AND ITS MIXTURES WITH STONE DUST

С.Б. Романченко, В.В. Соболев, Юрий Кузьмич Нагановский, Е.А. Губина
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Abstract

Представлены результаты экспериментального исследования пыли 7 марок углей по получению базовых термогравиметрических характеристик, а также сопоставительных экспериментов для состояния пыли до взрыва и после взрыва. Проведено выделение 4 представительных брутто-стадий термической деструкции угля и смесей. Отработаны методы термогравиметрического анализа (ТГА) для определения влажности образцов, аналитической зольности и стадийного выхода летучих веществ с разделением органической и негорючей газовых составляющих. Методом сопоставления ТГА характеристик определены стадии устойчивого снижения и стадии роста выхода летучих веществ при воздействии взрыва, позволяющие однозначно трактовать участие угольной пыли во взрыве, исследовать динамику фронта пламени. The article presents the results of an experimental study of dust of various grades of coal in order of increasing degree of metamorphism (D, DG, G, GZh, Zh, K, A) to obtain basic thermogravimetric characteristics. The samples were examined in an inert atmosphere with a change to an air atmosphere after the completion of coking. The temperature of the heating zone increased linearly with a heating rate DТо = 20 °C/min (the second mode is DТо = 100 °C/min) in the range from 25 °C to 850 °C. The mass of the sample was measured 30 times per minute. When 850 °C was reached, isothermal heating was carried out for 15 minutes until the coking process was completed, then the inert atmosphere was replaced with an air one in order to afterburn the coke and to determine the ash Ad. Additional comparative experiments were carried out for the state of dust «before the explosion» – «after the explosion». There was carried out the isolation of 4 gross stages of thermal destruction of coal and mixtures under the thermal effects of fire or explosion: the stage of analytical moisture release Wа(MRS – Moisture Removal Stage) from 25 °C up to 130 °C; the stage of «primary» volatiles release (PVS – Primary Volatiles Stage) from 400 °C up to 600 °C; the stage of «secondary» volatiles release (SVS - Secondary Volatiles Stage) from 600 °C up to 750 °C; the stage of carbon dioxide release in coal and stone dust mixtures (CDS – Carbon Dioxide Stage) from 700 °C up to 840 °C. It was determined that the maximum release rate of volatiles at the PVS stage is reached at a temperature of 465 °C – 505 °C, the presence and output value of volatiles at this stage determines the explosive properties of dust. The SVS stage exists in coals of a high stage of metamorphism and anthracites, however, the hazard of such dust from explosions has not been experimentally confirmed. There was carried out the study of dust after explosions in an explosive 20-liter chamber and dust collected in mines after explosions. For dust obtained from full–scale mine explosions, there was determined a sharp (in 3.5–5 fold) decrease in the residual volatile yield in the PVS stage with a simultaneous increase in the volatile yield at the SVS stage. And also there was determined the appearance of low-temperature differential thermogravimetry (DTG) peaks (at a temperature of 200 °C – 300 °C). Dust from 59 coal seams was examined, the total number of thermogravimetric studies was more than 150. The methods of selecting logically related dust samples at emergency sites during the elimination of explosions at mines (2013–2021) were tested. There were elaborated both stable method for numerical recognition of dust involvement in an explosion and methods of thermogravimetric analysis of coal and stone dust mixtures, and also the methods of retrospective analysis of the dynamics of explosion development during the investigation of technical factors of accidents in coal mines.
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煤尘及其与石粉混合物爆炸危险的热重实验研究
Представлены результаты экспериментального исследования пыли 7 марок углей по получению базовых термогравиметрических характеристик、在此基础上,我们还将继续努力,以确保在全球范围内,使我们的用户能够享受到更多的服务。Проведено выделение 4 представительных брутто-стадий термической деструкции угля и смесей.Отработаны методы термогравиметрического анализа (ТГА) для определения влажности образцов、аналитической зольности и стадийного выхода летучих веществ с разделением органической и негорючей газовых составляющих.Методом сопоставления ТГА характеристик определены стадии устойчивого снижения и стадии роста выхода летучих веществ при воздействии взрыва、позволяющие однозначно трактовать участие угольной пыли во взрыве, исследовать динамику фронта пламени.文章介绍了为获得基本热重特性而对各种等级的煤尘进行实验研究的结果,这些煤尘的变质程度依次为 D、DG、G、GZh、Zh、K、A。样品在惰性气氛中进行检测,焦化完成后转为空气气氛。在 25 °C 至 850 °C 的范围内,加热区的温度以 DТо = 20 °C/min 的加热速率线性上升(第二种模式为 DТо = 100 °C/min )。样品的质量每分钟测量 30 次。当温度达到 850 ℃ 时,进行 15 分钟等温加热,直到结焦过程结束,然后用空气取代惰性气氛,以便对焦炭进行后燃烧并测定灰分 Ad。此外,还对 "爆炸前 "和 "爆炸后 "的粉尘状态进行了对比实验。在火灾或爆炸的热效应下,对煤和混合物的热破坏的 4 个总阶段进行了分离:分析水分释放阶段 Wа(MRS - 除湿阶段),从 25 °C 至 130 °C;"一次 "挥发物释放阶段(PVS - 一次挥发物阶段),从 400 °C 至 600 °C;"二次 "挥发物释放阶段(SVS - 二次挥发物阶段),从 600 °C 至 750 °C;煤和石粉混合物中二氧化碳释放阶段(CDS - 二氧化碳阶段),从 700 °C 至 840 °C。据测定,PVS 阶段的最大挥发物释放率在温度 465 °C - 505 °C 时达到,该阶段挥发物的存在和输出值决定了粉尘的爆炸特性。SVS 阶段存在于变质程度较高的煤炭和无烟煤中,但这种粉尘的爆炸危险尚未得到实验证实。对 20 升爆炸室爆炸后的粉尘和矿井爆炸后收集的粉尘进行了研究。对于从大规模矿井爆炸中获得的粉尘,已确定在 PVS 阶段残余挥发物产量急剧下降(3.5-5 倍),同时在 SVS 阶段挥发物产量增加。此外,还发现出现了低温差热重(DTG)峰(温度为 200 °C - 300 °C)。对 59 个煤层的粉尘进行了研究,热重研究的总数超过 150 项。在消除矿井爆炸(2013-2021 年)期间,测试了在应急地点选择逻辑相关粉尘样本的方法。在调查煤矿事故的技术因素期间,详细制定了参与爆炸的粉尘数值识别稳定方法和煤与石粉混合物热重分析方法,以及爆炸发展动态回顾分析方法。
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