Zonal Evolution Mechanism and Coupled Superposed-Arch Bearing Effect in Loose-Fragmented Soft-Rock Roadways

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2026-03-31 DOI:10.1155/gfl/7819463
Jin Chen, Hengkai Wang, Zhonghua Wei, Qingli Gao
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Abstract

To effectively address the challenge of stabilizing roadways in loose and fractured rock masses, the 12810 transportation roadway of the Yunjialing Mine was selected as the engineering case. The modified Hoek–Brown criterion was employed to derive analytical expressions for the stress distribution in different zones of the surrounding rock and for the radius of the plastic zone, thereby revealing the key factors controlling roadway stability. Based on the postexcavation degradation characteristics, the surrounding rock was divided from the excavation boundary inward into a fractured zone, a plastic softening zone, and an elastic zone, and the corresponding control principles and key techniques for extremely fractured soft-rock roadways were proposed. On this basis, three major control measures were identified: restraining the expansion of the fractured zone through high-prestress support components, mobilizing the bearing capacity of the surrounding rock through an effective support-bearing zone, and reinforcing weak sections to form a continuous bearing ring. Accordingly, a full-section combined control scheme of “high-strength prestressed long-short cables plus floor destressing anchorage” was developed. Considering the characteristics of this support scheme and based on the Hoek–Brown criterion suitable for loose and fractured rock masses, a “coupled superimposed bearing arch” capable of achieving both internal and external load bearing was proposed. This coupled bearing arch unifies the interaction between the support system and the surrounding rock with the radial confining force provided by the support, significantly amplifying the load-bearing capacity of rock bolts and cables. The results indicate that the extent of the fractured zone decreases with increasing uniaxial compressive strength and geological strength index (GSI) of the surrounding rock. Progressive expansion and transformation of the boundary between the fractured zone and the plastic softening zone is identified as the fundamental cause of large-scale rock mass fragmentation and bolt/cable anchorage failure. After applying the combined control scheme, deformation of the 12810 roadway was effectively controlled: The total convergence of the sidewalls was approximately 362 mm, roof subsidence about 142 mm, floor heave about 215 mm, and no large-scale cable ruptures occurred, ensuring roadway stability.

Abstract Image

松散破碎软岩巷道分带演化机制及叠拱耦合承载效应
为有效解决松散破碎岩体中巷道的稳定问题,选取云家岭矿12810运输巷道作为工程实例。采用改进的Hoek-Brown准则,推导了围岩不同区域应力分布及塑性区半径的解析表达式,揭示了控制巷道稳定性的关键因素。基于开挖后围岩的退化特征,从开挖边界向内将围岩划分为破碎区、塑性软化区和弹性区,并提出了相应的极端破碎软岩巷道控制原则和关键技术。在此基础上,确定了三种主要控制措施:通过高预应力支护构件抑制裂隙区扩展,通过有效的支护承载区调动围岩承载力,加强薄弱段形成连续承载环。据此,提出了“高强预应力长短索+底板减压锚固”的全断面组合控制方案。考虑该支护方案的特点,基于适用于疏松破碎岩体的Hoek-Brown准则,提出了一种既能承受内外荷载的“耦合叠加支承拱”。这种耦合拱将支护系统与围岩的相互作用与支护提供的径向围力统一起来,显著提高了锚杆和锚索的承载能力。结果表明:随着围岩单轴抗压强度和地质强度指数(GSI)的增大,裂隙带的范围减小;断裂区与塑性软化区边界的逐步扩展和转变被认为是大规模岩体破碎和锚索锚固破坏的根本原因。采用联合控制方案后,12810巷道变形得到有效控制:侧壁总收敛约362 mm,顶板沉陷约142 mm,底鼓约215 mm,未发生大规模拉索断裂,巷道稳定。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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