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