首页> 外文会议>New development on engineering blasting. >Basic Characteristics of the Stages of Rock Massif Destruction by Explosive Crushing
【24h】

Basic Characteristics of the Stages of Rock Massif Destruction by Explosive Crushing

机译:爆炸压碎破坏岩石地块阶段的基本特征

获取原文
获取原文并翻译 | 示例

摘要

For definition of the most essential characteristics of mechanical interaction of the explosion products with environment it is possible to consider according to the C. I. Petrovsky model three-stage destruction of strong rock mass by explosion of blasthole charges. At the first stage the powerful compression wave, formed by explosion, destroys rock on the contact "charge-environment", from the crushing zone border the zone of radial cracks spreads. In the beginning process differs a little from the phenomena accompanying explosion in the boundless environment, but interaction of compression wave with a free surface leads to more intensive crushing of massif. This stage is short-term, but during this time the most part of energy of explosives is spent During this stage basic destruction of the breaking layer is carried out and inducer cavity of cylindrical form reaches the limited volume. At the second stage owing to a free surface influence axially symmetrical development of cavity is broken. Caseous products of explosion impart to the destroyed part of massif the accelerated movement towards a free surface. Action of the explosion products remained in a cavity is the main defining factor at this stage. The third stage is inertial scattering of rock in the gravity field, formation of disintegration of the broken rock. By our theoretical researches it was defined that the basic physical characteristic of the first stage is the limited radius of the explosive cavity, which take into account end result of explosion action in rock. The main physical characteristic of the second and the third stages is initial speed of movement of the centre of mass of the blown up part as predetermining rocks interposition in disintegration. In the paper the analytical dependences are adduced for definition of the indicated characteristics. They interconnect the sought characteristics with elastic and strength properties of rocks, with the detonation, physical and chemical characteristics of applied explosive and parameters of the charge location in massif.
机译:为了定义爆炸产物与环境的机械相互作用的最基本特征,可以根据C.I. Petrovsky模型,通过爆炸孔炸药对强岩体进行三阶段破坏。在第一阶段,由爆炸形成的强大的压缩波破坏了接触“装料-环境”上的岩石,从破碎区边界的径向裂缝开始扩散。在开始的过程中,与无边环境中伴随爆炸的现象略有不同,但是压缩波与自由表面的相互作用导致了块体的更强烈地破碎。这个阶段是短期的,但是在此期间,炸药的大部分能量都被消耗掉了。在这个阶段中,对破坏层进行了基本破坏,圆柱形的诱导腔达到了有限的体积。在第二阶段,由于自由表面的影响,空腔的轴向对称发展被打破。爆炸的干酪状产物加速了向自由表面的运动,从而将其破坏了。在这个阶段,残留在腔中的爆炸产物的作用是主要的决定性因素。第三阶段是岩石在重力场中的惯性散射,形成破碎岩石的崩解。根据我们的理论研究,第一阶段的基本物理特征是爆炸腔的有限半径,其中考虑了岩石爆炸作用的最终结果。第二阶段和第三阶段的主要物理特征是爆破部分的质心的初始运动速度,这是预先确定岩石在崩解中的位置。在本文中,分析依赖性被用来定义所指示的特性。它们将所寻求的特性与岩石的弹性和强度特性,爆炸,所施加炸药的物理和化学特性以及在地块中的装药位置参数联系在一起。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号