论爆破地震波在传播过程中的衰减特性

    ON ATTENUATING CHARACTERISTIC OF BLASTING SEISMIC WAVES IN PROPAGATING PROCESS

    • 摘要: 爆破地震波能量随着传播距离的增加而不断衰减,其衰减程度主要受到传播介质的影响。以层状岩体为例,从理论上说明爆破地震波沿岩层走向、倾向传播时其强度衰减不同的原因。对比分析顺层山坡露天矿生产爆破震动效应试验的振动速度实测数据发现,在与爆源距离相同的条件下,爆破地震波在岩层的倾向上的衰减比走向要快,且在爆源距相等时,平行走向的振动速度是垂直走向的1.5~2.0倍。

       

      Abstract: With the spread distance increasing,the energy of blast earthquake wave will decrease.The media in which it spread mainly decides this process.Take layered rock for example,the essay theoretically explains the reason that earthquake wave reduced along the creation and inclining direction.Contrast anslysis of blast vibration in opencast shows,under the same blast distance,the earthquake wave in creating direction will attenuate more quickly than that in inclining direction.Even the same blast hole,the velocity paralleling to creating direction is 1.5 to 2 times than that when vertical to creating direction.

       

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