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Assessment of compression extent of rock mass.

Assessment of compression extent of rock mass.

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Due to the weakness in mechanical properties of chlorite schist and the high in situ stress in Jinping II hydropower station, the rock mass surrounding the diversion tunnels located in chlorite schist was observed with extremely large deformations. This may significantly increase the risk of tunnel instability during excavation. In order to assess...

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... maximum deformation of many sections after the primary support reached 0.5e0.7 m, which is 7.6%e10.6% of the radius of tunnel. Hoek and Brown (1980) and Barla (1995) have proposed assessment methods (see Table 4) of compressive deformation of rock mass based on empirical statistical data of large deformation of soft rocks. The method proposed by Hoek and Brown (1980) is adopted in the present study due to its advantage in classification. ...

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... The results of rock specimen tests show [52][53][54][55] that for mudstone, siltstone, argillite, and sandstone with a uniaxial strength of 25-40 MPa, the failure criterion for strain is about 0.02-0.03. Therefore, in the numerical simulation, the post-peak limit was accepted in the range of "−0.02"-"+0.02". ...
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... According to the Equations (B.6) and (B.7), 2 ′ 0 equals to the sum of radial stress and tangential stress at node B. Thus, the evolution of the stress state at node B should be Line-1. Owing to the node being in the elastic state, the tangential stress can be calculated as Equation (2). In addition, the stress state moving along line-1 does not accumulate plastic shear strain. ...
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... ( Figure 3). Tis corresponds with the results of testing soft rock specimens in a volumetric feld [36][37][38] and under uniaxial compression [39,40]. According to the results of tests, it was found that for mudstone, siltstone, argillite, and sandstone with uniaxial strength of 25-40 MPa, the failure criteria for strain is about 0.02-0.03. ...
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... Technical difficulties, delays, economic repercussions and health and safety risks have occurred at many engineering projects developed on complex formations (Goodman and Ahlgren, 2000;Lunardi et al., 2014;Medley, 2007Medley, , 2001. These difficulties have encouraged both private and public institutions to develop and fund several research projects all over the world during the 40 years (e.g., the Italian Research Council (C.N.R.) (D'Elia et al., 1998), the California Department of Water Resource's Division of Safety of Dams -DSOD, see (Lindquist, 1994a;Medley, 1994), the National Natural Science Foundation of China, see (Huang et al., 2021;Wang, 2014;Yang et al., 2019;Zhou et al., 2014), and the Alexander von Humboldt Foundation, see (Kahraman and Alber, 2008), to better understand the geotechnical behavior of heterogeneous formations with a block-in-matrix fabric. ...
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The terms “bimrocks”, “bimsoils” and “soil-rock mixtures” indicate different and very common types of geological units with a block-in-matrix fabric that are also “geotechnically complex formations” and are characterized by an internal heterogeneity, and spatial variability of mechanical parameters and lithological compositions. Due to this internal complexity, the understanding of their geomechanical behavior presents a key challenge in geotechnical engineering. However, the lack of a standardized and clear terminology complicates the discrimination of different types of complex formations and their internal mechanical properties, which leads to inconsistency in the literature and research studies. This inconsistency causes misunderstandings, with possible practical implications for the characterization, analysis, design and construction of engineering works. By a combination of geological and geotechnical observations, we propose a new classification for geotechnically complex formations, with particular attention to those with a block-in-matrix internal fabric. Four properties are at the base of this new classification and have a primary role in controlling the geotechnical behavior of block-in-matrix units (bimunits): (i) the composition (i.e., lithology, degree of lithification/consolidation, nature, and rheology) of blocks and the matrix that affects the water sensitivity, (ii) the degree of internal anisotropy (DA) of the block-in-matrix fabric, (iii) the degree of stratal disruption and mixing, and (iv) the volumetric block proportion (VPB). As a result, we classified bimunits in those with “anisotropic”, “isotropic”, and “mixed” (i.e., different behavior depending on the DA of the matrix) textures and, each of these types, into block-in-matrix rocks and block-in-matrix soils (bimrocks and bimsoils in the following). According to the water sensitivity of the matrix, bimrocks are also differentiated into “hard” and “soft”. The novelty of the classification is that it is not limited to few types of geotechnically complex formations (e.g., flysch) but it can be easily applied to all field-based investigations of the different types of complex formations, regardless of their internal degree of stratal disruption, composition, and mechanical response to water sensitivity.
... The long-term behavior and stability of rock engineering structures such as tunnels have received considerable attention (Jia et al. 2020;Do et al. 2020;Sharifzadeh and Tarifard 2014;Pellet et al. 2009). A significant number of engineering applications and laboratory studies indicated the mechanical response related to weak and soft rock's time-dependent behavior is relatively complicated Yan et al. 2020;Török et al. 2019;Singh et al. 2018;Patil et al. 2018;Vlastelica et al. 2018;Lyu et al. 2017;Günther et al. 2015;Miščević and Vlastelica 2014;Zhou et al. 2014). One of the significant parameters affecting the underground spaces' longterm stability is weak rock mass creep response (Kovačević et al. 2021;Panthi and Shrestha 2018). ...
... It is in good agreement with previous works, where time-dependent changes in viscoelastic rock masses and the interaction of liners were studied (Do et al. 2020). The introduction of underground water strongly modifies the system's stability, especially when weak rocks are present (Zhou et al. 2014). In our study, the tunnel crown is stable in the case of rock mass creep behavior, but by introducing underground water and in the case of water table equals 40 m, the pressures created by axial force and bending moment are too considerable for the tunnel crown to sustain (Table 5 and Fig. 8). ...
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The time-dependent stability of tunnels is an important and challenging topic, mainly when the tunnel is excavated in incompetent and weak rocks. The creep property of rock is one of the crucial mechanical properties of weak rock and the main factor affecting the long-term stability of rock masses. Also, water as an important environmental factor influences both the short-term and long-term behavior of rocks and is one of the causes of geotechnical engineering disasters, such as tunnel collapse, slope sliding, surface subsidence, etc. In this research, the effects of rock’s creep behavior and underground water on the long-term stability of the Shibli tunnels were analyzed. Geological maps and reports of Shibli tunnels show a highly jointed condition in the surrounding rocks which have been crushed by two orogenic stages. The Burger-creep visco-plastic model was used to simulate the tunnel host rock creep behavior. The model's parameters were adopted based on the displacement-based direct back analysis technique using a univariate optimization algorithm. In addition, the influence of underground water is assessed under the condition of the varying water table. Support capability diagrams were used to evaluate the loading created on the tunnel’s permanent lining due to the creep behavior of rock mass and underground water. This study suggests that the weak rock's creep behavior and underground water significantly affect the time-dependent stability of tunnels. Results show that the induced stresses due to the rock's creep behavior and underground water are more considerable in the tunnel spring-line. Also, the increasing 20 m in the water table approximately decreases ten years of tunnel lining stability time at the fault zone. Article highlights Rocks creep behavior and underground water significantly affect the time-dependent stability of tunnels in weak rocks. Displacement-based direct back analysis using a univariate optimization algorithm was used to determine the CVISC model’s properties. Increasing 20 m in the water table approximately decreases ten years of tunnel lining stability time at the fault zone.