Rockslide as a Geophysical Process of Rock Bump or Sudden Outburst of Rock and Gas

S. Bychkov
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Abstract

Millions of years of atmospheric, biochemical, catagenetic, metamorphic, radioactive, and other gases under the influence of rock pressure and other physico-chemical factors, were introduced into the rocks of the earth's crust and mantle year after year. During absorption, the crystal lattices of the rocks were deformed with a change in their size and shape, and the molecules of the rocks and gases formed stable chemical compounds - solid solutions [1-3]. Practice shows that under normal conditions, the reverse process - the degassing of rocks, stretches for thousands of years, which allows the crystal lattices without plastic fracture to change their sizes and shapes. But, as practice shows, at some random moment, it is possible to start the process of avalanche-like degassing of a block of rocks. After a sudden outflow of gases, the crystal lattices of the rocks must take on a natural configuration, but due to the high rate of deformation, the relaxation process cannot keep up with the increase in stress. There is a collapse of the crystal lattices with the release of energy expended by nature on their deformation and the occurrence of elastic impacts - impulses, which are known in mining practice as rock bump and sudden outburst of rocks and gas. This process is possible in the event of a chain chemical reaction in a rock mass triggered by high-energy molecules, ions, and free radicals, similar to the so-called Cold Explosion process, which was discovered in 1980 at the Institute of Chemical Physics of the USSR Academy of Sciences. The reaction mechanism of the Cold Explosion is explained by the appearance of giant deformation loads in the sample arising from the rapid cooling of the sample. During the collapse, the process of high-speed degassing plays the role of cooling, and the mechanism of the chain chemical reaction is explained by the interaction of free radicals, high-energy molecules, and other charged particles in accordance with N. Bohr's postulates. A description of the mechanism of large-scale rock-slide and the process of formation of high-energy molecules, ions, free radicals according to the principle scheme X → X • + + e¯ / Y + e¯ → Y necessary for starting a chain chemical reaction in rock massif and the physico-chemical conditions accompanying the process is devoted this article.
岩石滑动是岩石碰撞或岩石与气体突然突出的地球物理过程
数百万年来,在岩石压力和其他物理化学因素的影响下,大气、生化、变质、放射性等气体,年复一年地被引入到地壳和地幔的岩石中。在吸收过程中,岩石的晶格发生变形,大小和形状发生变化,岩石分子与气体分子形成稳定的化合物——固溶体[1-3]。实践表明,在正常条件下,相反的过程——岩石的脱气过程持续了数千年,这使得没有塑性断裂的晶格可以改变其大小和形状。但是,实践表明,在某个随机的时刻,有可能开始像雪崩一样对一块岩石进行脱气。在气体突然流出后,岩石的晶格必须呈现自然形态,但由于高变形率,松弛过程不能跟上应力的增加。由于自然界消耗的能量的释放,晶体晶格的变形和弹性冲击-脉冲的发生,即在采矿实践中被称为岩石碰撞和岩石和气体的突然突出。这一过程可能发生在由高能分子、离子和自由基引发的岩体链式化学反应中,类似于1980年在苏联科学院化学物理研究所发现的所谓冷爆炸过程。冷爆炸的反应机理可以用试样在快速冷却过程中产生的巨大变形载荷来解释。在坍缩过程中,高速脱气过程起到冷却的作用,链式化学反应的机理根据玻尔假设由自由基、高能分子和其他带电粒子的相互作用来解释。本文描述了大规模岩石滑坡的机理,描述了在岩体中发生链式化学反应所必需的X→X•+ + e¯/ Y + e¯→Y原理格式下高能分子、离子、自由基的形成过程及伴随此过程的物理化学条件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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