露天矿高台阶抛掷爆破粉尘运移及粒径分布规律研究

Migration and particle size distribution of high-bench throwing-blasting dust in open-pit mines

  • 摘要: 露天矿高台阶抛掷爆破粉尘扩散动力学行为与常规爆破粉尘存在本质差异,然而现有数值模型多基于常规爆破条件建立,尚未针对抛掷爆破粉尘的特性进行调整与准确描述,且数值模拟的关键输入参数缺乏充足的现场实测数据支撑,制约了模拟结果的预测精度与工程适用性。针对上述问题,通过高速摄影观测技术进行了现场监测,结果表明:粉尘运移过程可划分为冲击运动阶段、“蘑菇云”形成阶段和扩散运动阶段;爆破后粉尘浓度呈先迅速升高再持续波动最终衰减的变化趋势;粉尘以中等颗粒(粒径为20~100  μm)为主,累计占比为56.2%,细颗粒(粒径<20  μm)累计占比为34.4%,粗颗粒(粒径>100  μm)累计占比仅为9.4%。建立了露天矿高台阶抛掷爆破粉尘运移三维几何模型,使用Fluent软件进行了粉尘运移瞬态数值模拟,结果表明:① 在初始快速释放阶段,粉尘受重力和惯性力主导作用呈现出高度聚集的分布特征;随后进入持续输运阶段,粉尘在浮力及环境风场作用下显著抬升和横向扩展;最终进入扩散沉降阶段,粉尘因重力沉降和湍流扩散稀释导致整体浓度显著降低。② 粗颗粒粉尘快速沉降,中等颗粒粉尘随风流迁移,细颗粒粉尘长时间悬浮并远距离输运。

     

    Abstract: High-bench throwing blasting dust in open-pit mines exhibits essential differences in diffusion dynamics compared with conventional blasting dust. However, existing numerical models are mostly established under conventional blasting conditions and have not been adjusted or accurately characterized to capture the characteristics of throwing blasting dust. In addition, key input parameters for numerical simulations lack sufficient field-measured data support, which restricts the prediction accuracy and engineering applicability of simulation results. To address these problems, field monitoring was conducted using high-speed photographic observation technology. The results showed that the dust migration process could be divided into an impact motion stage, a "mushroom cloud" formation stage, and a diffusion motion stage. After blasting, dust concentration first rose rapidly, then fluctuated continuously, and finally decayed. Dust was dominated by medium-sized particles (20–100 μm), accounting for 56.2% of the cumulative proportion; fine particles (<20 μm) accounted for 34.4%; and coarse particles (>100 μm) accounted for only 9.4%. A three-dimensional geometric model of dust migration from high-bench throwing blasting in open-pit mines was established, and transient numerical simulations of dust migration were carried out using Fluent. The results indicated that ① during the initial rapid-release stage, dust exhibited highly aggregated distribution characteristics under the dominant effects of gravity and inertial forces; subsequently, during the sustained transport stage, dust was significantly lifted and expanded laterally under the effects of buoyancy and ambient wind fields; and finally, in the diffusion–settling stage, overall dust concentration decreased markedly due to gravitational settling and dilution by turbulent diffusion. ② Coarse dust particles settled rapidly, medium dust particles migrated with the airflow, and fine dust particles remained suspended for a long period and were transported over long distances.

     

/

返回文章
返回