我国煤岩动力灾害模拟试验仪器研制现状与关键难题

Instruments for simulation experiments on coal-rock dynamic disasters in China: Current status and key challenges

  • 摘要:
    背景 煤岩动力灾害是采动扰动作用下煤岩层多相多场耦合失稳导致的工程灾害,严重制约深部资源安全开采。阐明煤岩动力灾害机理是探索有效监测预警与防控技术的基础,而模拟试验仪器则是研究其致灾机理的重要工具。随着科技水平的逐渐提高,我国自主研制的模拟试验仪器在不断完善和进步,而随着工程活动逐渐向深部发展,深部地层的多相多场赋存环境对模拟试验仪器的功能与结构提出了更高的要求。
    方法 利用CiteSpace软件系统梳理我国近50年来煤岩动力灾害模拟试验仪器研制相关文献,从仪器结构与功能、多场环境模拟、监测装置与方法等3个方面系统总结仪器的发展趋势及研制现状。
    结果和结论 我国煤岩动力灾害模拟试验仪器经历了单向、双向及三向加载的发展历程,实现了煤岩层真实三向应力环境的模拟,通过引入动载扰动模块,设计出动静组合式真三轴加载结构,实现了对各类工程采动扰动的模拟。仪器可模拟的多场环境从单一的应力场逐步发展为“流−固”耦合两场(应力场、渗流场)、“热−固−流”耦合多场,逐步实现真实地层复杂多物理场环境的模拟。监测装置与方法由常规的应力应变监测逐步发展为多元信息监测,实现灾变过程孕灾及前兆信息的精准捕获。深地工程处于复杂的多相多场孕灾环境,现有仪器仍然难以真实还原这种复杂孕灾环境,煤岩动力灾害模拟试验仪器未来需突破3个关键难题,一是设备结构与功能需实现地层真实应力环境及多应变率工程扰动的模拟;二是需实现应力场、渗流场、温度场等多场耦合环境的原态模拟;三是需发展动态捕获多场参数演化的监测装置与方法,引入人工智能相关技术手段,实现灾变过程原场再现。

     

    Abstract:
    Background Coal-rock dynamic disasters represent engineering disasters caused by the instability of the multi-phase and multi-field coupling of coal strata under mining disturbances, severely restricting the safe exploitation of deep coal resources. Elucidating the disaster-inducing mechanisms lays the foundation for exploring effective monitoring and early warning, along with prevention and control technologies, while instruments for simulation experiments provide crucial tools for investigating the mechanisms. Gradually increasing scientific and technological level has contributed to the continuous improvement in China's independently developed instruments for simulation experiments on coal-rock dynamic disasters. However, as engineering activities progressively extend toward deep parts, the multi-phase and multi-field coal occurrence environments in deep strata impose higher requirements for the instruments’ functions and structures.
    Methods  Based on the CiteSpace software, this study presents a review of literature on China’s development of instruments for simulation experiments on coal-rock dynamic disasters issued in the past 50 years. Accordingly, the development trends and current status of these instruments are comprehensively summarized from three aspects: structure and function, multi-field environment simulation, and monitoring devices and methods.
    Results and Conclusions  In China, instruments for simulation experiments on coal-rock dynamic disasters have evolved from uniaxial to biaxial and then to triaxial loading, enabling the simulation of the true triaxial stress environments of coal strata. By introducing a module of dynamic load disturbances, a static-dynamic combined true triaxial loading structure has been designed, supporting the simulation of various engineering disturbances in coal mining. The environments simulated by the instruments have transitioned from a single stress field to two fields with fluid-solid coupling (stress and seepage fields) and further to multiple fields with thermo-solid-fluid coupling, gradually achieving the simulation of complex multi-physical field environments in real strata. Furthermore, the monitoring devices and methods of the instruments have progressively advanced from conventional stress-strain monitoring to multi-dimensional information monitoring, allowing disaster-inducing and precursor information in the disaster evolution process to be accurately captured. Nevertheless, existing instruments still struggle to faithfully reproduce the complex multi-phase and multi-field disaster-inducing environments encountered by deep underground engineering. In the future, the instruments should overcome three key challenges. First, their structures and functions should allow for the simulation of both the real in-situ stress environments of strata and engineering disturbances with multiple strain rates. Second, they should support the in-situ simulation of environments with the coupling of the stress, seepage, and temperature fields. Third, it is necessary to develop monitoring devices and methods that enable the dynamic capture of information on the evolution of multi-field parameters and, by introducing technologies such as artificial intelligence (AI), to achieve the in-situ reproduction of the disaster evolution process.

     

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