A Deformation Control Method of Tunnel Surrounding Rock Applied to Granite Alteration Zone Under Seepage Conditions
A technology of surrounding rock deformation and control method, which is applied in the direction of tunnels, earthwork drilling, mining equipment, etc., can solve the problems of overall instability of excavation surface, increase of tunnel construction cost, multiple changes of support schemes, etc., and achieve economical support cost effect
Patent Information
- Authority / Receiving Office
- CN · China
- Patent Type
- Patents(China)
- Current Assignee / Owner
- Publication Date
- 2021-07-09
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Abstract
Description
technical field
[0001] The invention relates to tunnel engineering, in particular to a method for controlling deformation of tunnel surrounding rock applied to a granite alteration zone under seepage conditions. Background technique
[0002] Due to its special diagenetic process and evolution process, the rock mass in the granite alteration zone has special mechanical properties such as low strength, water swelling and strain softening. Insufficient understanding of the distribution laws and engineering characteristics of granite alteration zone rock mass often brings great difficulties to engineering design and construction. In actual tunnel engineering, the seepage of groundwater and the strain softening characteristics of surrounding rock materials are the most important factors affecting tunnel deformation. The body strength is low, and the montmorillonite in the montmorillonized altered rock has the characteristics of water absorption and swelling, which can loosen and...
Examples
Embodiment
[0032] Qingshui Tunnel is located in the Anping-Nuodong section from Hongtang to Cenxi section of the Luo (Yang) Zhan (Jiang) Railway. The entrance mileage is DK439+346, the exit mileage is DK442+782, and the total length is 3436m. It is the control project of the Yongcen section of the Luozhan Railway. one.
[0033] The strata of the underlying bedrock of the tunnel are mixed in sequence, and the underlying bedrock is late Yanshanian granite and middle Ordovician Suoweiling Group sandstone interbedded with shale, limestone and marble formed by hydrothermal alteration. Among them, the granite is strongly weathered and varied, the rock mass is broken, the fully weathered layer is 35-80m thick, the rock core is soil columnar, silt-like, and spherical weathered bodies can be seen locally, which belongs to the granite alteration zone mentioned in this patent.
[0034] Section DK442+633~+782 crosses a long flowing gully and is located in the low and gentle area at the foot of the m...