Based on the characteristics of strata movement of solid backfilling mining technology, the surface subsidence prediction method based on the equivalent mining height theory was proposed, and the parameters selection ...
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Based on the characteristics of strata movement of solid backfilling mining technology, the surface subsidence prediction method based on the equivalent mining height theory was proposed, and the parameters selection guideline of this method was also described. While comparing the parameters of caving mining with equivalent height, the subsidence efficient can be calculated according to the mining height and bulk factor of sagging zone and fracture zone, the tangent of main influence angle of solid backfilling mining is reduced by 0.2-0.5(while it cannot be less than 1.0). For sake of safety, offset of the inflection point is set to zero, and other parameters, such as horizontal movement coefficient and main propagation angle are equal to the corresponding parameters of caving mining with equivalent height. In the last part, a case study of solid backfilling mining subsidence prediction was described. The results show the applicability of this method and the difference of the maximum subsidence point between the prediction and the observation is less than 5%.
为研究徐州冬季雾-霾天气形成过程中颗粒物粒径及气溶胶光学特性的变化特征,分析了2014年12月1日-2015年2月28日徐州大气颗粒物质量浓度(PM(10)、PM(2.5)、PM1)、数浓度(0-1μm、1-2.5μm、2.5-10μm)和气溶胶光学特性等数据.结果表明:0-1μm粒径范围细颗粒物的大量增多是引发徐州冬季雾-霾天气的主要因素,徐州冬季地面风速小(静风或轻风天气),较高的大气相对湿度对雾-霾的形成和维持起着重要影响作用.持续时间较长的雾霾天气,因颗粒物吸湿增长和水汽附着,1-10μm粒径范围大气颗粒物在雾霾时段易发生沉降而减少,后随相对湿度降低雾霾转为短时间的霾天气,1-10μm颗粒物数浓度大幅上升.徐州冬季500nm波段AOD total和AOD fine mode具有相同的变化趋势,雾-霾日AOD total和AOD fine mode显著高于非霾日.AOD fine mode与AOD coarse mode的比值雾-霾日亦明显高于非霾日,而且在雾-霾日Angstrom波长指数主要集中在1-1.6,表明徐州冬季雾-霾时段大气中细颗粒物为主控粒子.
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