岩土力学 ›› 2026, Vol. 47 ›› Issue (3): 856-868.doi: 10.16285/j.rsm.2025.0632CSTR: 32223.14.j.rsm.2025.0632

• 基础理论与实验研究 • 上一篇    下一篇

变温−水冷循环作用下极硬花岗岩力学损伤特性及贯入性研究

蒋亚龙1, 2,周亚风1,徐彭楚璇1,张旗3, 4,邱思宝1   

  1. 1. 华东交通大学 山区土木工程安全与韧性全国重点实验室,江西 南昌 330013;2. 中国矿业大学 深地工程智能建造与健康运维全国重点实验室,江苏 徐州 221116;3. 武汉大学 土木建筑工程学院,湖北 武汉 430072;4. 武汉大学 岩土与结构工程安全湖北省重点实验室,湖北 武汉 430072
  • 收稿日期:2025-06-17 接受日期:2025-10-15 出版日期:2026-03-17 发布日期:2026-03-18
  • 通讯作者: 张旗,男,1989年生,博士,副教授,主要从事岩石破裂过程及震源机制反演等研究工作。E-mail: zhqi@whu.edu.cn
  • 作者简介:蒋亚龙,男,1991年生,博士,教授,主要从事TBM滚刀破岩机制与数值模拟研究。E-mail: yalongjiang@whu.edu.cn
  • 基金资助:
    国家自然科学基金(No.42377169);江西省自然科学基金(No.20232BCJ23004);第八届青年人才托举工程(No.2022QNRC001);中国博士后科学基金(No.2025T180885;2024M750898);深地工程智能建造与健康运维全国重点实验室项目(No.SDGZK2409)。

Mechanical damage and penetrability of extremely hard granite subjected to thermal-shock cycles using water cooling

JIANG Ya-long1, 2, ZHOU Ya-feng1, XU Peng-chu-xuan1, ZHANG Qi3, 4, QIU Si-bao1   

  1. 1. National Key Laboratory of Safety and Resilience in Mountain Civil Engineering, East China Jiaotong University, Nanchang, Jiangxi 330013, China; 2. State Key Laboratory of Intelligent Construction and Healthy Operation and Maintenance of Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, China; 3. School of Civil Engineering, Wuhan University, Wuhan, Hubei 430072, China; 4. Key Laboratory of Geotechnical and Structural Engineering Safety of Hubei Province, Wuhan University, Wuhan, Hubei 430072, China
  • Received:2025-06-17 Accepted:2025-10-15 Online:2026-03-17 Published:2026-03-18
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (42377169), the Natural Science Foundation of Jiangxi Province (20232BCJ23004), the Young Elite Scientists Sponsorship Program by CAST (2022QNRC001), the China Postdoctoral Science Foundation (2025T180885, 2024M750898) and the State Key Laboratory of Intelligent Construction and Healthy Operation and Maintenance of Deep Underground Engineering (SDGZK2409).

摘要: 在地下工程领域,研究全断面掘进机(tunnel boring machine,简称TBM)热损伤破岩技术时,传统的等温循环方案存在高能耗问题,极大地制约了其经济性及未来应用推广。为了应对这一难题,探索变温−水冷循环这一新型热加载方式对岩石的劣化效应,对于推动该技术的节能降耗与工程应用具有重要价值。通过开展单轴压缩、巴西劈裂及贯入试验,系统研究了极硬花岗岩经历3次不同高温(T1、T2、T3)水冷循环后的可掘性变化,分析了岩石破裂模式、形态、抗压强度、抗拉强度及贯入速率的演化规律。研究结果表明:随着初始温度T1的升高,岩石热致微裂纹由稀疏分布逐渐发展为网状分布,并由仅晶间裂纹扩展形成损伤破坏,破裂模式由劈裂拉伸转变为斜面剪切,破坏形态呈现脆性向延性过渡的特征,其中500 ℃为关键转折点;岩石强度的下降速率及贯入速率的提升率在T1处于500~600 ℃范围内达到最大,之后逐渐减缓并趋于稳定;当T1> 600 ℃后,贯入速率的提升幅度较600 ℃时有所减缓,但其绝对贯入性仍高于常温对照组;第2次高温T2(200~600 ℃)虽能进一步降低岩石强度、增大热致微裂纹密度和破碎区体积,但其对破裂模式与形态的影响弱于T1;贯入速率在T2为200 ℃时出现显著提升。因此,在极硬岩层TBM掘进中采用变温−水冷辅助破岩时,推荐采用初始高温600 ℃、后续200 ℃的循环方案。

关键词: 变温?水冷循环, 极硬岩, 力学强度, 破坏模式, 贯入试验

Abstract: In the field of underground engineering, the traditional isothermal cycle scheme employed in TBM-assisted thermal damage rock breaking technology is hampered by high energy consumption, which severely limits its economic viability and future application. To address this challenge, investigating the rock degradation effect induced by a novel variable temperature-water cooling thermal loading method is of significant value for promoting energy efficiency and practical implementation of this technology. Through uniaxial compression, Brazilian splitting, and penetration tests, this study systematically investigated the evolution in penetrability of extremely hard granite subjected to three cycles of variable temperature-water cooling at different high temperatures (T1, T2, T3). The analysis focused on the evolution of rock failure patterns, morphology, compressive and tensile strength, and penetration rate. The results indicate that as the initial temperature T1 increases, thermally induced microcracks evolve from a sparse to a networked distribution, with damage initiated solely through intergranular crack propagation. The failure mode transitions from tensile splitting to oblique shear, accompanied by a brittle-to-ductile shift in failure morphology, with 500 ℃ identified as the critical transition point. Both the rate of strength reduction and the rate of penetration increase peak within the T1 range of 500−600 ℃, beyond which they gradually decelerate and stabilize. When T1 exceeds 600 ℃, the rate of penetration increase diminishes compared to that at 600 ℃, although the absolute penetrability remains superior to the room-temperature control group. While the second high-temperature stage T2 (200−600 ℃) further reduces rock strength and increases microcrack density and crushed zone volume, its influence on failure mode and morphology is less pronounced than that of T1. A significant enhancement in penetration rate is observed specifically when T2 is 200 ℃. Therefore, for TBM excavation in extremely hard rock formations utilizing variable temperature-water cooling assistance, a cyclic scheme with an initial high temperature of 600 ℃ followed by a subsequent temperature of 200 ℃ is recommended.

Key words: variable temperature-water cooling cycle, extremely hard rock, rock strength, failure mode, penetration tests

中图分类号: TU443
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