真三轴应力状态下煤与瓦斯突出两相流L型巷道运移特性试验研究

Experimental study on migration characteristics of coal and gas outburst two-phase flow in L-shaped roadway under true triaxial conditions

  • 摘要: 煤与瓦斯突出两相流具有强大的冲击动力作用,对井下人员和设备造成严重的损害。为了充分认识煤与瓦斯突出两相流的运移规律及致灾机制,利用多场耦合煤矿动力灾害大型物理模拟试验系统开展了真三轴应力状态下煤与瓦斯突出物理模拟试验,分析了煤与瓦斯突出两相流在L型巷道中的运移特性及其冲击特性。结果表明:在L型巷道中,突出煤粉流在主巷段中存在射流、稀相流和密相流3种流动状态。受直角拐弯结构影响,仅有少量的突出煤粉进入支巷段,主要分布在直角拐弯结构前端,表明拐弯结构大幅度抑制了煤粉的流动。突出煤粉以粒径小于0.15 mm的颗粒为主,其在巷道内的运移可分为初始加速、二次加速、衰减3个阶段,初始阶段煤粉流速度最高可达25.0 m/s。在突出过程中,巷道内煤与瓦斯两相流冲击力呈现出迅速增加-缓慢衰减的演化趋势。冲击力达到峰值后并不是平滑地下降,而是1个存在多峰值的震荡衰减过程,表明突出具有阵发特性。在主巷段中,最大冲击力沿巷道呈现波动式分布特征。随着传播距离的增加,增长区的持续时间逐渐增大,冲击力的衰减程度逐渐降低。煤与瓦斯两相流的冲击破坏特性主要体现在其前中部,距离突出口2、6和8 m处皆存在对人体造成严重损伤的风险。随着突出的发展,冲击力致灾区域由巷道前部逐渐向中部发展。在支巷段中,两相流冲击力出现明显的陡增现象,呈强-弱交替分布,说明直角拐弯结构增强了两相流动力致灾程度。

     

    Abstract: Coal and gas outburst two-phase flow has a strong impact dynamic effect, which could cause seriousinjuryto underground personnel and damage to equipment. In order to fully understand the migration law and disaster-causing mechanism of coal and gas outburst two-phase flow, a physical simulation test of coal and gas outburst under true triaxial conditions was carried out by using a large physical simulation test system of multi-field coupling coal mine dynamic disaster. The migration characteristics and impact characteristics of coal and gas outburst two-phase flow in aL-shaped roadway were analyzed. The results show thatin the L-shaped roadway, there are three flow states of jet, dilute phase flow and dense phase flow in the main roadway. Affected by the right angle turning structure, only a small amount of pulverized coal enters the branch roadway, mainly distributed at the front end of the right angle turning structure, indicating that the turning structure greatly inhibits the flow of pulverized coal. The pulverized coal is mainly composed of particles with a particle size of less than 0.15 mm. Its migration in the roadway can be divided into three stages:initial acceleration, secondary acceleration and attenuation. The maximum velocity of pulverized coal flow in the initial stage can reach 25.0 m/s.In the process of outburst, the impact force of coal and gas two-phase flow in the roadway presents an evolutionary trend of rapid increase and slow attenuation.After the impact force reaches the peak, it does not decrease smoothly, but it is a shock attenuation process with multiple peaks, indicating that the outburst has intermittent characteristics. In the main roadway, the maximum impact force presents a fluctuating distribution along the roadway. With the increase of the propagation distance, the duration of the growth zone gradually increases, and the attenuation of the impact force gradually decreases. The impact damage characteristics of coal and gas two-phase flow are mainly reflected in its front and middle parts.There is a risk of serious injury to human body at 2, 6 and 8 m away from the outburst place.With the development of the outburst, the disaster-causing area ofimpactforce gradually develops from the front of the roadway to the middle. In the branch roadway, the impact force of two-phase flow increases sharply, showing a strong-weak alternating distribution, which indicates that right angle turning structure enhances the dynamic disaster-causing degree caused by two-phase flow.

     

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