针对牡绥线双丰隧道穿越第三系砂泥岩的涌水涌泥问题,通过专项勘察、超前地质预报及室内试验、原位试验等方法,研究了涌水涌泥段的地质构造、水文地质情况及第三系砂泥岩的工程特性,并分析了第三系砂泥岩地层的失稳模式和涌水涌泥机理。结果表明:受开挖扰动地下水大量渗入,致使砂泥岩结构破坏并失稳;拱顶支护不足以支撑砂泥混合物与抗拒动、静水压力而产生变形,最终在薄弱处发生涌水涌泥。采用超前注浆加固及锚杆支护、泄水减压、三台阶临时仰拱+中立柱支护等措施治理后效果良好,双丰隧道得以在涌水涌泥段安全贯通。
Gushing water mud in the tertiary sand-mudstone stratum around the Shuangfeng tunnel on MUSUl hne is an engineering problem. The geological structure and hydrogeology condition at the gushing water mud section, and engineering characteristic of the tertiary sand-mudstone stratum were studied through specific survey, advanced geological prediction,lab test and in-situ test. The instability mode and the mechanism of the gushing water mud of the tertiary sand-mudstone stratum were studied. The results show that the significant penetration of underground water due to excavation disturbance may result in the damage of sand-mudstone stratum structure and the lack of stability. The vault supporting is not appropriate for the mixture of sand and mud, and the static and dynamic water stress, and it deforms accordingly. Eventually, gushing water mud occurs at the weakest point. There are some effective measures including pre-grouting and rock bolting, discharge decompression, three steps of temporary inverted arch plus center pillar. In this way, the gushing water mud problem around Shuangfeng tunnel was solved.