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<title>China Journal of Highway and Transport-Channel: Tunnel Engineering</title>
<description>Channel: Tunnel Engineering</description>
<link>http://zgglxb.chd.edu.cn</link>
<language>EN-US</language>
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<title><![CDATA[Heat Transfer Characteristics and Temperature Field Evolution Laws: Field Experiments of Tunnel in Cold Areas Under Annual Cycles]]></title>
    <link><![CDATA[http://zgglxb.chd.edu.cn/EN/abstract/abstract4459.shtml]]></link>
<description><![CDATA[Addressing the insufficient understanding of the temperature field evolution laws of tunnels in cold areas, this study performed an analysis of the annual periodic tunnel heat transfer characteristics. The Yejishan Tunnel was taken as a case study, and field experiments were conducted to examine the variation patterns of air temperature along the tunnel longitudinal length and the temperature field of the lining and surrounding rock along the tunnel radial depth. Factors, such as external meteorological conditions, burial depth, initial temperature of the surrounding rock, and thermal properties of the lining and surrounding rock, were considered, thus determining the evolution laws of the tunnel temperature field. The findings indicate that the Yejishan Tunnel is predominantly affected by the wind-wall differential pressure, resulting in a dominant airflow from the inlet to the outlet. As the distance from the inlet increases, the air temperature in the tunnel increases gradually during winter, with the annual average air temperature also increasing. The variation pattern along the tunnel length is significantly impacted by the longitudinal distribution of the tunnel burial depth. For the Yejishan tunnel, the annual average air temperature essentially follows an exponential function distribution along the tunnel length with respect to the burial depth. The annual air temperature amplitude decreases exponentially. Influenced by the annual average air temperature and initial temperature of the surrounding rock, the annual average temperature logarithmically increases with radial depth, approximating the initial temperature of the surrounding rock. As radial depth increases, the influence of air temperature fluctuations reduces, and the annual temperature amplitude decays according to an exponential function. At a certain depth, such as 14-16 m in the Yejishan tunnel, the annual temperature amplitude drops below 0.05 ℃, reaching the temperature influence boundary of the surrounding rock. Lower thermal conductivity of the lining or surrounding rock and shallower temperature influence depth of the surrounding rock accelerates the increase of the annual average temperature in the tunnel radial depth. Lower thermal diffusivity also results in a faster decay of the annual temperature amplitude and a shallower temperature influence depth of the surrounding rock. These factors influence the variation pattern of the tunnel temperature field along the radial and the maximum freezing depth of the surrounding rock. The frost damage prevention and control design of tunnel in cold areas should comprehensively consider the external meteorological conditions, tunnel trend, burial depth, initial temperature of surrounding rock, as well as the thermal properties of lining and surrounding rock.]]></description>
<category><![CDATA[Channel: Tunnel Engineering]]></category>
<author><![CDATA[CHEN Jian-xun, ZHAO Peng-yu, LUO Yan-bin, CHEN Li-jun, WANG Chuan-wu, XUN Wen-jie, DONG Ti-jian]]></author>
<pubDate><![CDATA[2023-09-09 00:00:00.0]]></pubDate>
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<title><![CDATA[Study on the Resilient Structure Design of Shield Tunnels]]></title>
    <link><![CDATA[http://zgglxb.chd.edu.cn/EN/abstract/abstract4460.shtml]]></link>
<description><![CDATA[The main structure of shield tunnels is usually constructed with assembled segmental linings. Shield tunnels exhibit complex mechanical behavior during disasters and are vulnerable and difficult to repair. It is reasonable to develop a resilience design to improve the anti-disaster capability of shield tunnels. This paper presents a structural resilience design against the structural feature and disaster characteristics of shield tunnels. The fortification target for shield tunnel structural resilience design is proposed, and the resilience limit states were defined based on a comprehensive consideration of the resilience fortification category, working condition, disaster damage, economic loss, and repair difficulty. On this basis, a system of resilience design indicators was established based on structural redundancy, robustness, resilience, and economy. Then, considering the bearing capacity and normal use limit state, the redundancy and robustness indicators were refined for strength, deformation, and crack control. Moreover, the corresponding control equation is proposed. The performance function of resilience design and the calibration process of partial coefficient were established based on reliability. Finally, a design and evaluation method was established for the resilience design of shield tunnel structures that can provide reference for the resilience design of tunnel structures and related research.]]></description>
<category><![CDATA[Channel: Tunnel Engineering]]></category>
<author><![CDATA[XIAO Ming-qing, FENG Kun]]></author>
<pubDate><![CDATA[2023-09-09 00:00:00.0]]></pubDate>
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<title><![CDATA[Study on Flow Plasticity and Permeability Characteristics of Foam-slurry-polymer Conditioned Coarse-grained Soil]]></title>
    <link><![CDATA[http://zgglxb.chd.edu.cn/EN/abstract/abstract4461.shtml]]></link>
<description><![CDATA[During earth pressure balance shield tunneling in the coarse-grained soil stratum with rich water, water spewing often occurs, and the use of foam for soil conditioning alone cannot guarantee anti-permeability of the soil. In particular, bentonite slurry can enhance the water plugging effect and stability of foam. However, under the condition of high water pressure and coarse-grained soil, slurry is easily lost; thus, the addition of a polymer is required to condition soil. Accordingly, in this study, slump and permeability tests were carried out for foam-bentonite slurry-polyacrylamide (PAM) conditioned gravelly sand. The results indicate the difficulty for the foam and bentonite slurry with little viscosity to remain in the large pores of gravelly sand, and the conditioned soil was granular with slurry and foam loss. Whereas, with addition of the polymer, the soil particles were aggregated, the internal friction angle of the soil was reduced, the plasticity and fluidity of the conditioned soil were improved, and no slurry or foam was lost. When the polymer content was low, the bentonite slurry and foam easily was discharged from the soil, the permeability coefficient of the conditioned soil exceeded 10<sup>-4</sup> m·s<sup>-1</sup> in a short time. This does not meet the anti-permeability requirement that a permeability coefficient of less than 10<sup>-5</sup> m·s<sup>-1</sup> should be stable for more than 90 min during shield tunneling. Increasing polymer content could lengthen the initial stable period of the permeability coefficient, and significantly reduce it when permeation tended to be stable. The permeability coefficient was stable below 10<sup>-5</sup> m·s<sup>-1</sup> for a long time, and the higher the polymer content, the more obvious the effect of permeability coefficient reduction. The conditioned soil with suitable flow plasticity might not have suitable permeability. It was suggested that the flow plasticity and permeability of soil should be evaluated synthetically considering shield tunneling in the coarse-grained soil stratum with rich water. Finally, the foam-slurry-polymer composite conditioning mechanism was achieved, confirmed via optical microscopy observation. Foam alone or foam and bentonite slurry cannot effectively condition the test soil, the viscosity of bentonite slurry can be improved by the polymer, effectively dispersing the condition agents in the pores of soil, and the foam stability can be enhanced through slowing down of foam drainage besides coarsening and coalescing by the polymer, so the flow plasticity and the permeability of soil can be conditioned appropriately.]]></description>
<category><![CDATA[Channel: Tunnel Engineering]]></category>
<author><![CDATA[WANG Shu-ying, CHEN Yu-jia, ZHONG Jia-zheng, LING Fan-lin]]></author>
<pubDate><![CDATA[2023-09-09 00:00:00.0]]></pubDate>
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<title><![CDATA[Study on Meter-level Large Deformation Mechanism of Soft Rock Mass Around Tunnel with High In-situ Stress]]></title>
    <link><![CDATA[http://zgglxb.chd.edu.cn/EN/abstract/abstract4462.shtml]]></link>
<description><![CDATA[Meter-level severe deformation disasters frequently occur due to deep-buried soft rock mass under high in-situ stress; however, the catastrophe mechanism and process of such large deformation is unclear. The combined finite-discrete element numerical method (FDEM) was employed to study the fracture and swelling deformation process of soft rock mass with high in-situ stress, and the influences of the in-situ stress value, the lateral pressure coefficient, and the shape of the tunnel section on the catastrophic mechanism of large deformation were investigated. The results indicate that the mechanism of large deformation catastrophe of soft rock mass with high in-situ stress involves the expansion of broken rock fragments induced by the unloading during tunnel excavation. Additionally, analyses of the fracture development process, stress field, and displacement field of the surrounding rock mass show that under hydrostatic pressure, the surrounding rock mainly produces conjugate shear failures, and these rock fragments slip along the main shear zone, accompanied by dilatancy and overturning motion, creating a large number of gaps between the fragments. The movement of these broken rock blocks into the tunnel space results in a sharp reduction of the tunnel section, followed by a meter-level severe deformation disaster. It was further found that as the in-situ stress increases, the fracture degree of surrounding rock mass and the maximum displacement at the tunnel surface increase rapidly. The latter exhibits obvious nonlinear characteristics, while the radius of the excavation damage zone increases relatively slowly. When the vertical in-situ stress is as high as 58 MPa, it is difficult for the rock mass in the severe displacement zone to form a main shear zone. The extremely cracked rock masses are squeezed into the tunnel as a whole, and a large number of voids are generated, resulting in a sharp reduction in the cross-sectional of the tunnel. Moreover, under hydrostatic pressure, the square tunnel only affects the crack initiation, the shape of the severe displacement zone, and the displacement mode of the rock mass in this zone. Outside of the severe displacement zone, the surrounding rock approaches the fracture mechanism of a circular tunnel.]]></description>
<category><![CDATA[Channel: Tunnel Engineering]]></category>
<author><![CDATA[DENG Peng-hai, LIU Quan-sheng]]></author>
<pubDate><![CDATA[2023-09-09 00:00:00.0]]></pubDate>
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