摘要:
水环境的改变是诱发黄土隧道灾害的主要因素,而优势通道的存在对于围岩中水分入渗起到重要作用。以偏桥隧道为工程背景,在现场调研的基础上,通过开展物理模型试验和数值模拟探究了降雨期间优势通道的演化过程、入渗特征及隧道结构响应规律,进一步揭示了裂隙优势入渗诱发黄土隧道变形破坏机理。结果表明:优势通道的孕育发展是“新”裂隙的形成与“旧”裂隙的延伸扩大共同耦合作用下的结果。在优势通道影响下,入渗模式从稳态入渗逐渐转变为裂隙控制的优势流入渗,改变围岩水分迁移路径的同时加快了水分渗入深部围岩。随着裂隙深度的增加,优势渗流影响范围越来越大,浸润锋形态逐渐由“曲线型”变为“漏斗型”。裂隙末端形成的局部暂饱和区加剧了围岩变形,使得隧道受力表现出明显的不对称性,其中优势运移通道下侧隧道结构所受影响最为突出。当出现贯通裂隙时,优势入渗所引起的隧道拱顶沉降达到56.3 mm,结构应力增值相较于均匀入渗增大140 kPa。
Abstract:
The change of water environment is the main factor inducing loess tunnel disasters, and the existence of dominant channels plays an important role in the infiltration of water into the surrounding rock. Taking the Pianqiao Tunnel as the engineering background, based on on-site research, the evolution process, infiltration characteristics of dominant channels, and tunnel structural response laws during rainfall were explored through physical model experiments and numerical simulations, further revealing the deformation and failure mechanism of loess tunnels induced by crack dominant infiltration. The results indicate that the development of dominant channels are the result of the coupling effect of the formation of "new" cracks and the extension and expansion of "old" cracks. Under the influence of dominant channels, the infiltration mode gradually changes from steady-state infiltration to fissure controlled dominant infiltration, changing the migration path of surrounding rock water while accelerating water infiltration into deep surrounding rock. As the depth of the crack increases, the range of influence of dominant infiltration becomes larger, and the infiltration front gradually changes from "curved" shape to "funnel-shaped" shape. The local temporary saturation zone formed at the end of the crack intensifies the deformation of the surrounding rock, resulting in a significant asymmetry in the stress distribution of the tunnel, with the tunnel structure under the dominant channels being most affected. When a through crack appears, the settlement of the vault caused by dominant infiltration reaches 56.3 mm, and the structural stress increases by 140 kPa compared to uniform infiltration.