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液态二氧化碳相变爆破射流形态演变和温度分布特性研究

Investigation of morphological evolution and temperature distribution properties of liquid carbon dioxide phase change blasting jet

  • 摘要: 作为炸药破岩技术的有力替代,CO2相变爆破破岩技术的理论研究长期滞后于现场实践,而CO2相变爆破产生的射流是致裂岩体的根本动力。基于CO2致裂技术裂岩原理,以CO2超高度欠膨胀射流为理论基础,通过高速红外相机及高速相机,构建了同时捕捉CO2射流结构与射流温度分布的CO2爆破射流全过程测试系统,研究了不同剪切片厚度下不同型号致裂器爆破射流演化特征。研究结果表明:CO2爆破初期射流为典型的超高度欠膨胀射流,射流具有高度的非稳定性,在不同的阶段表现出不同的射流形态特征,其中95型致裂器初期爆破射流形状受膨胀波影响较大,由椭圆形演变为近似球体。射流演化过程具有复杂的相态变化,CO2相变爆破射流整体上经历喷射启动、动态扩展、稳定发展后,最终形成气−固两相混合的复杂流动状态。随着剪切片厚度的增加,同一时刻可见云轴线扩散长度增大,但扩散能力的边界增益减弱,同时射流轴线可见云扩散峰值速度增大。射流温度分布具备明显的阶段特征,在高温膨胀阶段,射流核心温度急剧升高,超过温度捕捉上限184.133 ℃,导致射流角度增大至近180°。随着剪切片厚度的增加,CO2爆破射流超温区域的持续时间及“超温像素点”占比出现增大趋势。研究结果为进一步深入探索CO2爆破射流破岩机理提供了基础数据及试验支撑。

     

    Abstract: Research on CO2 phase change blasting has historically fallen behind field practice as a powerful alternative to explosive rock-breaking technology. The jet generated by CO2 phase change blasting serves as the primary force behind the fracturing of rock mass. A comprehensive CO2 blasting jet test system was developed, utilizing high-speed infrared and standard high-speed cameras, based on the principle of rock splitting in CO2 fracturing technology and the ultra-high under-expansion jet of CO2. The research explored the characteristics of blasting jets as they evolved from various types of fracturing devices across different shear thicknesses. The results show that the initial jet of CO2 blasting represents a typical ultra-high under-expansion jet, characterized by significant instability and varying morphological features at different stages. The shape of the initial blast jet of the Type 95 fracturing device is notably influenced by the expansion wave, transforming from an oval to an approximately spherical shape. The evolution of the jet encompasses intricate phase changes. The CO2 phase change blasting jet experiences injection initiation, dynamic expansion, and stable development, resulting in a complex flow of a gas-solid two-phase mixture. As the thickness of the shear slice increases, the diffusion length of the visible cloud axis also expands, whereas the boundary gain of the diffusion capacity diminishes. Furthermore, the maximum diffusion velocity along the jet axis increases. In the high-temperature expansion phase, the core temperature of the jet rises dramatically, surpassing the temperature measurement limit by 184.133 ℃, resulting in the jet angle approaching nearly 180°. As the shear slice thickness increases, both the duration of the over-temperature region and the proportion of 'over-temperature pixels' in the CO2 blasting jet rise accordingly. This study offers essential data and experimental backing for additional exploration of the rock-breaking mechanisms associated with CO2 blasting jets.

     

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