煤与瓦斯突出的扩容突变机理

Mechanism of dilatation catastrophe of coal and gas outburst

  • 摘要: 煤与瓦斯突出机理作为百年世界性难题,其防治在现阶段已进入瓶颈期。面对突出事故的不间断发生,其背后所涉及的众多科学问题仍难以解答,如地应力与瓦斯压力及煤体力学强度在突出孕育过程中的耦合作用和主控阶段性特征尚未能明晰。为此,基于典型突出事故所被触发的力学背景,从采动煤体力学损伤动态响应规律入手,揭示了多变力学行为下含瓦斯煤体损伤过程中的扩容特征,明晰了采动应力与瓦斯压力互馈响应规律,阐明了孕突过程中煤体初始破坏主控机制,进而提出了煤与瓦斯突出的扩容突变机理。结果表明:含瓦斯煤体损伤失稳过程所凸显的扩容特征分为扩容缓增、扩容快增、扩容突增及扩容骤增4个阶段,期间瓦斯压力因地应力作用先后经历作用能力强化增强阶段(扩容缓增阶段)、作用能力强化减弱阶段(扩容快增阶段和扩容突增阶段)及作用能力弱化阶段(扩容快增阶段后或扩容突增阶段后或扩容骤增阶段后)。而煤体原始强度并不能决定实际煤体破坏程度,甚至破坏的难易程度,关键在于应力加卸载路径。突出的本质则是含瓦斯煤岩体在地应力与瓦斯压力主控作用阶段性转变过程中,由煤体发生扩容突变现象引发结构失稳并被抛出的一个具有典型时间属性的突变动力过程(称为突出的“扩容突变机理”)。一次突出的孕育过程可分为3个阶段:首先煤体在以地应力为主导、瓦斯压力协同作用下发生初始损伤(扩容缓增阶段与扩容快增阶段),称为突出孕育的第1阶段;而后煤体在以瓦斯压力为主导、地应力协同作用下发生结构分区层裂化,并产生进一步碎裂(扩容突增阶段和扩容骤增阶段),称为突出孕育的第2阶段;最后层裂煤体在瓦斯压力的作用下发生破碎及粉化(即扩容突变),称为突出孕育的第3阶段。进而破碎煤体在瓦斯压力的作用下被抛出,激发突出。研究成果为煤与瓦斯突出机理认识的深化提供了新的视野,同时可为突出防治技术革新奠定理论基础。

     

    Abstract: Coal and gas outburst mechanism, as a century old global problem, has entered a bottleneck period in its prevention and control at this stage. Faced with the continuous occurrence of outburst accidents, it is still difficult to answer numerous scientific questions behind them, such as the coupling effect among in situ stress, gas pressure, and coal mechanical strength in the process of outburst incubation, and the characteristics of the main control stages are not yet clear. Therefore, based on the mechanical background triggered by typical outburst accidents, starting from the dynamic response law of mechanical damage in mining coal masses, in this work the dilatation characteristics in the process of coals damage are revealed, clarifying the law of mutual feedback response between mining stress and gas pressure. And the main control mechanism of initial failure of coals in the process of an outburst incubation. Then the dilatation catastrophe mechanism of coal and gas outburst is proposed. The results show that the dilatation characteristics in the damage and instability process of coal containing gas can be divided into four stages: slow dilatation, rapid dilatation, sudden dilatation, and surged dilatation. And the gas pressure undergoes the enhancement of strengthening action ability (slow dilatation), the decrease of strengthening action ability (rapid dilatation and sudden dilatation), and and the weakening gas pressure action ability (after rapid dilatation, or sudden dilatation, or surged dilatation). The original strength of coals cannot determine the actual degree of coal failure, or even the difficulty of failure. The key lies in the stress loading and unloading path. The essence of an outburst is a sudden change dynamic process with typical time attributes (known as the “dilatation catastrophe mechanism” of outburst) that occurs because of dilatation catastrophe phenomenon of coal containing gas during the phased transformation process of main controlling action between in situ stress and gas pressure, causing structural instability of coals and being ejected out. The incubation process of an outburst can be divided into three stages: firstly, the coal masses undergo initial damage (slow dilatation and rapid dilatation) under the dominant action of in situ stress with the assistance of gas pressure, which is called the first stage of outburst incubation; Then, the coal masses undergo regional spallation under the dominant action of gas pressure with the synergistic effect of in situ stress, and further fragmentation occurs (sudden dilatation and surged dilatation), which is called the second stage of outburst incubation; Finally, under the action of gas pressure, the fractured coals undergo fragmentation and pulverization (i.e. dilatation catastrophe), which is called the third stage of outburst incubation. In turn, the fractured coals are thrown out under the action of gas pressure, triggering an outburst. The research results can provide a new perspective for deepening the understanding of coal and gas outburst mechanism, with laying a theoretical foundation for the innovation of outburst prevention and control technologies.

     

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