Investigation of Fracture Evolution and Failure Characteristics of Rocks under High-Temperature Liquid Nitrogen Interaction

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-10-17 DOI:10.1155/2023/6664383
Linchao Wang, Yi Xue, Xuyang Shi, Zhihao Zhang, Xue Li, Lin Zhu, Ruifu Liu, Lin Sun, Caifang Wu, Songbao Feng
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引用次数: 0

Abstract

The utilization of liquid nitrogen as a sustainable and water-free fracturing medium exhibits immense promise in engineering applications. In this investigation, Brazilian split tests and acoustic emission tests were conducted to explore the impact of liquid nitrogen cooling on the internal structure and mechanical properties of rock specimens. To examine the influence of liquid nitrogen cooling on the tensile strength of rocks, displacement-load curves were obtained from samples subjected to varying cycles of high-temperature liquid nitrogen cooling using Brazilian split tests. Acoustic emission experiments were conducted to investigate the characteristics of granite samples exposed to various cycles of high-temperature liquid nitrogen cooling. Based on these findings, the impact of liquid nitrogen cooling on the internal structure of rock masses was analyzed. The findings of this study demonstrate that high-temperature liquid nitrogen thermal treatment significantly modifies the microscopic structure and mechanical properties of rocks, with potential implications for overall stability and reliability. Notably, an observable decline in tensile strength was observed as the number of cycles of high-temperature liquid nitrogen treatment increased. These findings underscore the substantial impact of liquid nitrogen cooling on the behavior of rocks. High-temperature liquid nitrogen treatment effectively promotes the generation of microcracks within rocks, thereby increasing their permeability. During the experiment, granite specimens primarily exhibited shear-type fractures when subjected to high-temperature freeze-thaw cycles induced by liquid nitrogen.
高温液氮作用下岩石断裂演化及破坏特征研究
液氮作为一种可持续的无水压裂介质,在工程应用中具有巨大的前景。通过巴西劈裂试验和声发射试验,探讨液氮冷却对岩石试件内部结构和力学性能的影响。为了研究液氮冷却对岩石抗拉强度的影响,采用巴西劈裂试验对不同高温液氮冷却循环的样品进行了位移-载荷曲线分析。采用声发射实验研究了不同高温液氮冷却循环下花岗岩试样的声发射特性。在此基础上,分析了液氮冷却对岩体内部结构的影响。本研究结果表明,高温液氮热处理显著改变了岩石的微观结构和力学性能,对岩石的整体稳定性和可靠性具有潜在的影响。值得注意的是,随着高温液氮处理循环次数的增加,拉伸强度明显下降。这些发现强调了液氮冷却对岩石行为的重大影响。高温液氮处理有效地促进了岩石内部微裂纹的产生,从而增加了岩石的渗透率。实验中,花岗岩试件在液氮诱导的高温冻融循环作用下,主要表现为剪切型断裂。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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