Research on Rock Fracturing by High-Intensity Electric Shock Fracturing─A Perspective on Images of Fracture Surfaces

IF 5.2 3区 工程技术 Q2 ENERGY & FUELS
Baisheng Nie*, Zhehao Zhang*, Xirong He, Yilan Zhang, Xianfeng Liu and Xiaotong Wang, 
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引用次数: 0

Abstract

High-intensity electric shock (HES) is a new type of fracturing technology that uses electrical energy as a driver. Self-developed ultrahigh-power HES equipment is used to fracture rocks, which is to study the fracturing mechanism of HES. Strain curves of rock fracture processes and ultradeep field images of rock sections are used to analyze the force characteristics and fracturing process of rocks. The rock fracture process is subjected to intense strains with values exceeding 100,000. The generation of strains is related to tensile and shear stresses. The rock section mainly exhibits a tensile section texture. The main cause of rock fracture is the extension of fractures due to the destruction of grain boundaries and intergranular structures. The significance of the above findings is a clearer explanation of the rock-breaking mechanism of the HES.

Abstract Image

高强度电击(HES)是一种以电能为驱动力的新型压裂技术。利用自主研发的超高功率 HES 设备压裂岩石,研究 HES 的压裂机理。利用岩石断裂过程的应变曲线和岩石断面的超深场图像,分析岩石的受力特征和断裂过程。岩石断裂过程中会产生超过 100,000 的强烈应变。应变的产生与拉应力和剪应力有关。岩石断面主要呈现拉伸断面纹理。岩石断裂的主要原因是晶界和晶间结构的破坏导致断裂扩展。上述研究结果的意义在于更清晰地解释了高海拔地震的岩石破碎机制。
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来源期刊
Energy & Fuels
Energy & Fuels 工程技术-工程:化工
CiteScore
9.20
自引率
13.20%
发文量
1101
审稿时长
2.1 months
期刊介绍: Energy & Fuels publishes reports of research in the technical area defined by the intersection of the disciplines of chemistry and chemical engineering and the application domain of non-nuclear energy and fuels. This includes research directed at the formation of, exploration for, and production of fossil fuels and biomass; the properties and structure or molecular composition of both raw fuels and refined products; the chemistry involved in the processing and utilization of fuels; fuel cells and their applications; and the analytical and instrumental techniques used in investigations of the foregoing areas.
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