Piston mechanism of interaction of non-linear geomechanical and physicochemical gas exchange and mass transfer processes in coal-bearing rocks

T.A. Kiryaeva
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Abstract

The article focuses on a theoretical and experimental framework for the quantification of interaction between nonlinear geomechnical and physicochemical processes in high-stress coal-bearing rock mass during mining under high seismic risk due to large-scale blasting and earthquakes, as well as because of structural and temperature effects. The tests were aimed to examine and study comprehensively the piston mechanism of gas exchange and mass transfer processes, revealed recently at the Institute of Mining, SB RAS, as well as to explain the fact that the earthquake-induced low-velocity (quasi-meter range) pendulum waves (velocity to 1 ​m/s and frequency of 0.5–5 ​Hz) could stimulate an increase in the gas content in coal mines. In order to perform laboratory investigation at the Institute of Mining SB RAS, special-purpose stand for analyzing gas exchange and mass transfer processes in coal-bearing geomaterials under various thermodynamic conditions (P, V, T) and gas composition was constructed in cooperation with the Institute of Semiconductors Physics SB RAS. Matching of air flow rate with compression pressures allowed to obtain relations showing that air flow rate increases at the uncertain time interval under the increasing of the compression pressure. The same measurements was carried out with another gases such as Hydrogen H2, Helium He, methane CH4, carbon dioxide CO2 and carbon oxide CO. The laboratory tests aimed to detailed investigation of the previously revealed “piston mechanism” of gas exchange and mass transfer processes in the coal specimens and their quantitative description in terms of theory of the pendulum waves were carried in the first time. Consequently, there are some arguments for the testing of the opportunity of quantitative description of the “piston mechanism” related to gas exchange and mass transfer processes in the scale of coal mines. It is relevant when pendulum waves induced by powerful earthquakes and technical blasting reaches the mine.

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含煤岩石非线性地质力学与物理化学气体交换与传质过程相互作用的活塞机制
本文建立了一个理论和实验框架,用于量化在大规模爆破和地震以及结构和温度影响下高应力煤岩体开采过程中非线性地质力学和物理化学过程之间的相互作用。该试验旨在全面考察和研究SB RAS矿业研究所最近公布的气体交换和传质过程的活塞机制,并解释地震诱发的低速(准米范围)摆波(速度为1 m/s,频率为0.5-5 Hz)可以刺激煤矿瓦斯含量增加的事实。为了在中国矿业科学院进行实验室研究,与中国矿业科学院半导体物理研究所合作,建立了用于分析不同热力学条件(P、V、T)和气体成分下含煤岩土材料气体交换和传质过程的专用台架。将空气流量与压缩压力进行匹配,可以得到在不确定的时间间隔内,随着压缩压力的增大,空气流量增大的关系。对氢气H2、氦气He、甲烷CH4、二氧化碳CO2和氧化碳CO等气体进行了同样的测量。首次进行了室内测试,旨在详细研究之前发现的煤样气体交换和传质过程的“活塞机制”,并从摆波理论角度对其进行定量描述。因此,对于在煤矿尺度上对气体交换和传质过程的“活塞机制”进行定量描述的机会进行测试,存在一些争论。强地震和技术爆破引起的摆波到达矿山时具有一定的相关性。
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