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Interrelation of subsoil hydrogen emanation during bulk blasting and higher seismicity of the Khibiny massif

机译:散装爆破过程中地下土壤氢释放与Khibiny地块较高地震活动性之间的相互关系

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Currently ore mining in the mines of “Apatit” JSC is provided by intense underground andrnopen-pit mining works thus brings about its deepening and results in stress level and seismic activityrnincrease. The Khibiny apatite mines are characteristic of all types of rock pressure dynamicrnoccurrences: external prone-to-rockburst features to rockbursts and mining-induced earthquakes.rnBlock structures, high horizontal stresses, solid brittle rocks, dynamic occurrences of the rockrnpressure in the deep rock mass allow to refer developed mines as prone-to-rockburst or hazardousrnones. Stress-strained state of the rock mass is influenced by antropogenic and natural factors. As arnresult, a sudden block movement along the faults from one another or a new faulting inside the blocksrnor barrier opening between existing fractures take place; it results in seismic events of different energyrnlevels.rnThe important factor having impact on geodynamic situation in the region is the long-termrnantropogenic influence on the rock mass. As a result of ore mining and tailing dumps andrnimpoundments generation, the surface relief has changed significantly as well as type of loads on thernrockmass, tectonic elements relations were found destroyed thus leading to block system instabilityrnand seismic activity increase in the area of mining works.rnIndicators of geodynamic events can be gas components existing in any geological formations.rnGases, due its mobility, are very sensitive to changes in the host rock state. The prospects ofrnmolecular hydrogen emanation as precursors of natural and mining-induced processes were assessed.rnThis paper presents the study results of the interrelation of seismicity in the area of the UnitedrnKirovsky Mine and subsoil hydrogen emanation after blasting works in the mine. Obtained resultsrnproved the assumption that deep hydrogen emanation peaks following the bulk blasting coincide withrnthe further higher seismicity zone formation thus indicating the mining-induced character of thernKhibiny rock mass seismicity.rnInvestigations allowed to find seasonal character of intense gas emanation in time: during summerrnseason vibration frequency of H_2 concentrations significantly increases, independently of explosivernamount. This frequency can be connected with irregularity of the Earth’s rotation about its axes andrnaction of lunisolar tides. Intensity and instability increase of gas emanation is registered during newrnmoon and, in particular, full moon periods and often during the first and the last quarters of the moon.rnAt present time the studies are continued.
机译:当前,在“ Apatit”股份公司的矿山中,矿石的开采是通过大量的地下和露天开采来进行的,从而使其深化,并导致应力水平和地震活动的增加。 Khibiny磷灰石矿山是所有类型的岩石压力动态事件的特征:岩爆和采矿诱发的地震的外部易爆岩石特征:块状结构,高水平应力,固体脆性岩石,深部岩体中岩压的动态发生允许将已开发的地雷称为易爆岩爆或危险冰毒。岩体的应力应变状态受制于人为因素和自然因素的影响。结果是,沿着断层的断层突然发生移动,或者在现有裂缝之间的断层或屏障层内部发生了新的断层。影响该地区地球动力学状况的重要因素是对岩体的长期成岩作用。由于矿石开采,尾矿倾倒和蓄水的产生,地表起伏发生了巨大变化,岩体上的荷载类型也发生了变化,发现构造元素关系被破坏,从而导致了块体系统的不稳定性,并导致采矿工作区的地震活动增加。地质动力学事件可能是任何地质构造中都存在的气体成分。气体由于其流动性而对基质岩石状态的变化非常敏感。评估了氢分子释放作为自然和采矿诱发过程的前兆的前景。本文介绍了联合基洛夫斯基矿区地震活动性与矿山爆破后地下土壤氢释放之间的相互关系的研究结果。获得的结果证实了以下假设:大爆炸后的深部氢散发峰与更高的地震活动区形成一致,从而表明了Khibiny岩体地震活动的采矿诱发特征.rn研究允许及时发现强烈的气体散发的季节性特征:在夏季季节振动频率H_2的浓度显着增加,与爆炸物量无关。该频率可能与地球绕其轴的自转不规则以及日月潮汐的作用有关。在新月期间,尤其是在满月期间,通常在月球的第一和最后一个季度,记录了气体散发的强度和不稳定性。目前,研究仍在继续。

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