高地温矿井热−氧耦合对遗煤微观结构及自燃特性影响研究

Mechanism of thermal-oxygen coupling in high-temperature mines on microstructure and spontaneous combustion characteristics of residual coal

  • 摘要: 为深入揭示矿井高地温环境下热−氧耦合作用对遗煤微观结构及自燃特性的影响,以安徽新集二矿气煤为研究对象,综合运用多尺度表征手段与分子动力学模拟方法,研究经45 ℃、15 d热−氧耦合预处理后遗煤微观结构与自燃特性的演化规律。通过低温液氮吸附(BET)、X射线光电子能谱(XPS)、电子顺磁共振(EPR)、热重分析(TG)及锥形量热等先进试验手段,并结合Materials Studio分子动力学模拟,系统分析了热与氧在遗煤长期氧化过程中的独立贡献与协同效应。BET分析表明,热−氧耦合预处理促使煤样总孔体积增加27.78%,显著高于惰性气氛热处理的2.70%,证实氧气是孔隙结构扩展的主导因素;分子动力学模拟进一步揭示,热−氧耦合预处理煤样的氧气扩散系数较原煤提升773.59%,显著高于惰性气氛热处理煤样,从分子层面验证了氧气在增强孔隙传质能力中的关键作用。XPS分析显示,O/C原子比由原煤的0.93升至热−氧耦合预处理煤样的1.88,羧基碳(O—C=O)官能团相对占比由2.75%增至8.95%,表明热−氧耦合预处理显著促进了煤样表面氧化。EPR测试指出,热−氧耦合预处理煤样在氧化升温过程中的g因子与自由基浓度(Ng)均高于原煤与惰性气氛热处理煤样,自由基积累显著加剧。TG分析表明,热−氧耦合预处理煤样各特征温度(T1T6)较原煤均呈下降趋势,其中干裂温度(T2)降幅达33.10 ℃。锥形量热测试显示,点燃时间由原煤的84 s缩短至热−氧耦合预处理煤样的48 s,峰值热释放速率提升73.45%,总热释放量显著增加54.35%,煤样燃烧剧烈程度与火灾危险性显著上升。基于多尺度表征与模拟结果,构建了“孔隙扩展—表面氧化—自由基增殖—氧化加剧”的4级协同演化路径,从孔隙结构演变、表面化学活化、自由基链加速至热效应4个层面揭示了热−氧耦合驱动遗煤自燃的内在逻辑,为高地温矿井遗煤自燃风险防控提供了理论依据。

     

    Abstract: To thoroughly investigate the effects of thermal-oxygen coupling on the microstructure and spontaneous combustion properties of residual coal under high-temperature conditions in mines, this study focuses on gas coal from the Xinji No. 2 Mine in Anhui Province. By comprehensively employing multi-scale characterization techniques and molecular dynamics simulations, the study examines the evolution of the microstructure and spontaneous combustion properties of residual coal following 15 days of thermal-oxygen coupling pretreatment at 45 ℃. Using advanced experimental techniques such as low-temperature liquid nitrogen adsorption (BET), X-ray photoelectron spectroscopy (XPS), electron paramagnetic resonance (EPR), thermogravimetric analysis (TG), and cone Calorimetry, combined with Materials Studio molecular dynamics simulations, we systematically analyzed the independent contributions and synergistic effects of heat and oxygen during the long-term oxidation process of residual coal. BET analysis demonstrated that the thermal-oxygen coupling pretreatment increased the total pore volume of coal samples by 27.78%, significantly higher than the 2.70% observed in pure thermal pretreatment, confirming oxygen as the dominant factor in pore structure expansion. Molecular dynamics simulations further revealed that the oxygen diffusion coefficient of coal samples under thermal-oxygen coupling pretreatment increased by 773.59% compared to raw coal, markedly exceeding that of pure thermal pretreated samples, thereby validating the critical role of oxygen in enhancing pore mass transfer capacity at the molecular level. XPS analysis showed that the surface O/C atomic ratio increased from 0.93 in raw coal to 1.88 in thermal-oxygen coupled pretreated coal samples, while the relative content of carboxyl carbon (O—C=O) functional groups rose from 2.75% to 8.95%, indicating that thermal-oxygen coupling pretreatment significantly promoted surface oxidation of coal samples. EPR tests revealed that the thermal-oxygen coupled pretreated coal samples exhibited higher g-factor and free radical concentrations (Ng) during oxidation heating compared to raw coal and pure thermal pretreated samples, indicating significantly intensified free radical accumulation. TG analysis demonstrated a consistent downward trend in characteristic temperatures (T1T6) for thermal-oxygen coupled pretreated samples relative to raw coal, with the dry cracking temperature (T2) dropping by 33.10 ℃. Cone calorimetry tests showed the ignition time reduced from 84 seconds in raw coal to 48 seconds in thermal-oxygen coupled pretreated samples, while the peak heat release rate increased by 73.45% and the total heat release volume surged by 54.35%. These results indicate markedly enhanced combustion intensity and fire hazards. Based on the multi-scale representation and simulation results, a four-level synergistic evolution path of “porosity expansion-surface oxidation-radical proliferation-oxidation intensification” was constructed. The intrinsic logic of thermal-oxygen coupling-driven coal spontaneous combustion was revealed from four aspects: pore structure evolution, surface chemical activation, radical chain acceleration, and thermal effect. This provides a theoretical basis for the risk prevention and control of coal spontaneous combustion in high-temperature mines.

     

/

返回文章
返回