Coupled acoustic emission and petrographical insights into thermal degradation and fracture dynamics of an Indian sandstone

IF 4.9 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Shyam Raj Baloor, Kripamoy Sarkar, Dibyajeet Mohapatra, Bankim Chandra Mahanta, Tabish Rahman
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Abstract

Land subsidence induced by thermal stress degradation of rocks surrounding coal seams during the underground coal gasification (UCG) and underground coal-mine fire (UCF) constitutes a significant engineering geological hazard. The Jharia basin of India represents a critical case, as it is both a potential site for syngas production using the underground coal gasification techniques and is extensively affected by underground coal fire. To better understand the response of Jharia sandstone in extreme thermal environments, this research examines the physico-mechanical behaviour and fracture dynamics at various treatment temperatures between 25 °C and 800 °C. The research examines how grain size affects the strength and acoustic emission properties of sandstone at elevated temperatures. Crack initiation and damage thresholds were determined from linear-to-exponential trends in cumulative acoustic emission (AE) counts that marks the onset of stable microcrack nucleation. In contrast, crack damage stress threshold ratio indicates accelerated crack coalescence, evidenced by sharp increases in acoustic emission counts and energy. Microcracking initiated at 400 °C, and the strength parameters peaked when transgranular cracks were dominant. However, the strength parameters decreased significantly when the intergranular cracks were dominant at 600 °C. The grain-size and acoustic emission analyses revealed that the cumulative count and cumulative energy increased with increasing grain size. In contrast, the crack damage stress threshold showed an inverse relationship with the grain size.

印度砂岩热降解和裂缝动力学的耦合声发射和岩石学研究
煤矿井下气化和井下火灾过程中煤层周围岩石热应力退化引起的地面沉降是一种重大的工程地质灾害。印度的Jharia盆地是一个关键的例子,因为它既是使用地下煤气化技术生产合成气的潜在地点,又受到地下煤火的广泛影响。为了更好地了解Jharia砂岩在极端热环境下的反应,本研究考察了25°C至800°C不同处理温度下的物理力学行为和断裂动力学。该研究考察了晶粒尺寸如何影响高温下砂岩的强度和声发射特性。根据累积声发射(AE)计数的线性-指数趋势确定裂纹起裂和损伤阈值,这标志着稳定微裂纹成核的开始。相比之下,裂纹损伤应力阈值比表明裂纹加速合并,表现为声发射计数和能量的急剧增加。微裂纹在400℃时萌生,强度参数在穿晶裂纹占主导地位时达到峰值。而在600℃时,当晶间裂纹占主导地位时,强度参数明显下降。晶粒尺寸和声发射分析表明,累积计数和累积能量随晶粒尺寸的增大而增加。裂纹损伤应力阈值与晶粒尺寸呈反比关系。
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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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