Open Access
ARTICLE
Numerical Analysis of Temperature Field Distribution Characteristics of Surrounding Rock in Cross-Line Subway Tunnels
Aoyu Zheng1, Ye Wang1,2,*, Huanhuan Li1, Yuanfeng Lu1,3,*
1 School of Environmental and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou, China
2 Key Laboratory of Thermal Engineering of Railway Vehicles, Lanzhou Jiaotong University, Ministry of Education, Lanzhou, China
3 Infrastructure Department, Lanzhou University Second Hospital, Lanzhou, China
* Corresponding Author: Ye Wang. Email:
; Yuanfeng Lu. Email:
Frontiers in Heat and Mass Transfer https://doi.org/10.32604/fhmt.2026.075766
Received 07 November 2025; Accepted 19 January 2026; Published online 10 March 2026
Abstract
Subway operations generate substantial heat, and inadequate dissipation can progressively degrade tunnel thermal conditions. The thermal distribution within the surrounding rock is critical for calculating the load on subway environmental control systems. However, the heat transfer patterns in the surrounding rock for intersecting tunnels remain poorly understood. Therefore, this study employs COMSOL software to numerically analyze the impact of intersecting line layouts on the temperature field distribution within the surrounding rock. Results indicate that when tunnels intersect, heat accumulates in the surrounding rock near the intersection. Compared to the single-tunnel structure, intersecting tunnels exhibit higher peak temperature when reaching dynamic thermal equilibrium, and the time required to achieve equilibrium is longer. Reducing the vertical spacing between intersecting tunnels concentrates heat within the intersection zone, leading to elevated temperature in that area. However, when the vertical spacing exceeds 12 m, the numerical value no longer exhibits significant variation with vertical spacing. The intersection angle also influences the temperature distribution characteristic and numerical value. The smaller intersection angle causes heat to concentrate within the crossing zone, leading to an overall increase in surrounding rock temperature within that area. Additionally, the rate of temperature increase in the rock mass at the intersection zone and the magnitude of temperature at dynamic equilibrium are significantly influenced by geographical factors. The lower the ambient temperature in the climate zone where the intersecting subway tunnels are located, the faster the temperature rise rate at the intersection zone. When heat transfer in the rock mass reaches dynamic equilibrium, the temperature difference at the same monitoring point can reach approximately 10°C between severely cold and temperate regions.
Keywords
Subway tunnel; intersecting lines; surrounding rock and soil; temperature field; simulation modeling