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
网络首发:2026-03-18,
纸质出版:2026
移动端阅览
蒋亚龙, 周亚风, 徐彭楚璇, 等. 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[J]. 岩土力学, 2026,47(3):2025-11-25 11:13:24.
JIANG Ya-long, ZHOU Ya-feng, XU Peng-chu-xuan, et al. Mechanical damage and penetrability of extremely hard granite subjected to thermal-shock cycles using water cooling[J]. 2026, 47(3): 2025-11-25 11:13:24.
蒋亚龙, 周亚风, 徐彭楚璇, 等. 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[J]. 岩土力学, 2026,47(3):2025-11-25 11:13:24. DOI: 10.16285/j.rsm.2025.0632.
JIANG Ya-long, ZHOU Ya-feng, XU Peng-chu-xuan, et al. Mechanical damage and penetrability of extremely hard granite subjected to thermal-shock cycles using water cooling[J]. 2026, 47(3): 2025-11-25 11:13:24. DOI: 10.16285/j.rsm.2025.0632.
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(T、T、T)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T处于500~600 ℃范围内达到最大,之后逐渐减缓并趋于稳定;当T> 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T(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T;贯入速率在T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。
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 (T
T
T). 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 T 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 T range of 500−600 ℃
beyond which they gradually decelerate and stabilize. When T 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 T. A significant enhancement in penetration rate is observed specifically when T 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.
0
浏览量
122
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621