Field Tests on the Stress Characteristics of Enriched Water Tunnel Invert

Du, Mingqing; Li, Xiang; Wang, Xuchun; Teng, Hongwei; Zhang, Peng; Zhu, Zhen

doi:https://doi.org/10.1155/2021/6684884

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Coupled Mechanical and Hydraulic Properties of Fracture Networks

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Research Article | Open Access

Volume 2021 | Article ID 6684884 | https://doi.org/10.1155/2021/6684884

Field Tests on the Stress Characteristics of Enriched Water Tunnel Invert

Mingqing Du,¹Xiang Li,²Xuchun Wang,¹Hongwei Teng,¹Peng Zhang,¹and Zhen Zhu¹

Academic Editor: Feng Xiong

Received24 Dec 2020

Revised07 Jan 2021

Accepted13 Jan 2021

Published23 Jan 2021

Abstract

To monitor the changes in the force of the tunnel invert steel bars after the groundwater level changes, field tests were performed to accurately and comprehensively characterize the stress acting on the rebar of a tunnel invert. Changes in stress and temperature were monitored for two layers of rebar (upper and lower) in an actual tunnel invert during its repair. The results showed that the changes in stress followed different paths for the upper and lower layers. After the groundwater is replenished, the maximum tensile stress of the rebar was 17.3 MPa, and the maximum compressive stress was 120 MPa. Major changes in stress were observed 2–6 days after rain. Based on this, the seepage path of groundwater is analyzed. During this period, the compressive stress increased threefold, and the tensile stress increased 9.5-fold. The rebar stress in the tunnel invert followed a Gaussian distribution after stabilizing. Four phases of stress progression are identified and discussed. The results can provide data support and theoretical basis for the treatment of invert floor heave in enriched water tunnel.

1. Introduction

In recent years, the construction of high-speed railway has been accelerating. Especially in China, the mileage of high-speed railway has exceeded 35,000 km, which includes a large number of tunnels. An invert is an important part of a tunnel; its force and deformation directly determine whether a high-speed train can run safely and smoothly within the tunnel. Excessive force on the rebar is an important factor for invert floor heave; the change of groundwater level affects the force of invert. Problems with inverts have been widely reported in operational tunnels [1–3]. Thus, many studies have focused on the tunnel structure and surrounding rock failure. Tan et al. based on the Wangjing tunnel project studied the segment displacement and mechanical response of the shield tunnel with a diameter of 10.5 m in the process of shield construction and cross-passage construction [4]. Fang et al. and Zhang et al. calculated the seepage-induced effective stress around a tunnel in an elastic half-plane [5–7]. Li et al. defined a parameter called the partial failure ratio to describe the range of partial failure, which they used to analyze the limit support pressure and failure zone. Numerical simulations showed that their proposed model is very precise [8, 9]. Wen et al. established a flow-stress-damage model and its criterion of fracture expansion [10–12]. Li et al. carried out shear tests and sealed leakage tests on single fracture chlorite schist with or without grouting and evaluated strength and permeability of grouting effect [13–15].

Chiaia et al. introduced a suitable block model for evaluating the crack width and crack spacing of concrete structures with steel bars, which they extended to the serviceability stage of tunnel linings [16]. Kaya and Bulut applied a convergence confinement technique to check the capacity of suggested support units and used the 2D and 3D numerical finite element methods to determine the efficiency of the support design, dimensions of the plastic zones, and deformation [17]. Hu et al. studied the mechanical behavior of tunnel linings and found that the maximum positive bending moment and tensile cracks on the lining mainly develop in the direction normal to stratification [18]. Yoon et al. studied the effects of tunnel shapes on structural and hydraulic interactions and proposed a method for evaluating pore water pressure on tunnel linings [19]. Nematollahi and Dias used a finite difference code and nonlinear perfectly plastic constitutive model to study the structural forces induced on a tunnel lining [20]. Nogales et al. studied the mechanical properties of fiber-reinforced concrete in a tunnel lining [21, 22]. Meng et al. presented a novel 3D SRM mesoscale modeling method with concave particles and verified by experimental results [23–25].

Mou et al. studied 2D and 3D beam-column joints under pseudostatic loadings to investigate the influence of the loading type on seismic behavior, especially regarding the failure mode [26, 27]. Uenishi analyzed the scattering of a plane harmonic body wave by a uniformly lined circular tunnel and evaluated the possible mechanical characteristics of related incident seismic waves according to the failure mode of the structure [28]. Lv et al. and Huang et al. proposed stochastic damage models based on the micromechanical method for the bond stress-slip relationship of the interface under a monotonic load [29, 30]. Lin et al. studied reinforcement corroded to different levels and repeatedly loaded at different stress levels; their results showed that the bond behavior under cyclic loading is characterized by a progressive rise in the residual slip [31]. Campione et al. analyzed the experimental results of the local bond stress-slip relationship for steel bars embedded in lightweight fiber-reinforced concrete [32]. Xiao et al. analyzed the bond strength between recycled concrete and rebar and proposed a relationship between the stress and slip [33]. Wang et al. performed the pull-out test on 120 specimens; based on the results, they proposed a bond-slip constitutive model and a formula to represent the dissipated energy and elastic deformation energy [34].

Zhu et al. analyzed the effect of water-rock circulation on the mechanical properties of rock through a combination of macromechanical experiments and microstructure tests in the laboratory [35–39]. Zhang et al. performed laboratory tests and theoretical calculations to monitor a tunnel invert and clarified the definition and expression for the bearing capacity of a concrete-filled steel tube (CFST) supporting arch [40]. Kim et al. used laboratory tests and numerical analyses to study the behavior of a tunnel invert in weathered rock [41]. Seki et al. performed model experiments and numerical analysis to establish a rational measure of the heaving phenomenon [42]. Many other researchers have studied the mechanical characteristics and failure process of tunnel inverts through numerical analyses and experimental tests [43–47]. However, most research on inverts has only focused on the ultimate mechanical characteristics of the rebar. The process of changes in stress has been ignored, which is mainly because of the lack of data on the processes by which forces change. As an essential component of the invert structure, the rebar works with the concrete to bear the tensile stress of the invert and compensate for the low tensile strength of the concrete. Thoroughly understanding the stress characteristics and process of the reinforcement is very important for understanding the failure process and mechanism of the invert.

In this study, long-term field monitoring was carried out on the stress of the rebar in the invert of Fuchuan Tunnel of the Lanzhou–Urumqi High-Speed Railway. Meters were installed in the upper and lower rows of the rebar to obtain the changes in stress and temperature throughout the construction process from binding and concrete pouring to tunnel operation. The relationship between the rise of the groundwater level and the force of the invert was studied. The stress of the rebar was divided into four main phases to which different deformation control measures can be applied. This improves upon the current situation, where only the ultimate stress state is considered. The findings of this study will provide data and theoretical support for the deformation control of enriched water tunnel inverts.

2. Field Tests

2.1. General Situation

The invert at the DK41+410 section of Fuchuan Tunnel along the Lanzhou–Urumqi High-Speed Railway was chosen for the field test. Fuchuan Tunnel is in Gansu Province and has a total length of 10.65 km, maximum width of 14 m, and maximum height of 12.7 m. The invert has a concrete thickness of 55 cm and two rows of rebar. During the construction and operation of the tunnel, a large number of cracks appeared in the invert, as shown in Figures 1(a) and 1(b), which seriously affected the safe operation of trains. To accurately understand the internal stress of the invert, sensors were arranged on the rebar to monitor changes in stress as the tunnel was repaired. VWR-22 vibrating string extensometers, which can measure stress in the range of -200 to +300 MPa and temperature in the range of -40 to +150°C, were embedded in the upper and lower rebar layers of the invert directly below the center of the arch and slab track, as shown in Figure 2(a). Five points were monitored in each rebar layer, as shown in Figures 2(b)–2(d).

(a)

(b)

(a)

(b)

(c)

(d)

2.2. Analysis of the Test Results

Figure 3 graphs the stress and temperature of the rebar in the tunnel invert over time. Figure 3(a) shows the stress curve for the upper layer. The five monitoring points initially exhibited similar trends but diverged over time. The compressive stress initially decreased before increasing. Later, tensile stress appeared at the center of the invert and increased continuously, while the other four monitoring points showed that the compressive stress started increasing again. Figure 3(b) shows the corresponding curves for the lower layer. The compressive stress at the five monitoring points increased over time from concrete pouring to actual operation. Figure 3(c) plots the changes in temperature for the rebar. A large amount of hydrated heat was released after the concrete pouring, which caused the temperature of the material to initially increase before returning to room temperature. The rise and fall in temperature directly affected the compressive stress on the rebar. The field test data showed four distinct phases for the rebar in the tunnel invert from concrete pouring to actual operation: (1) the stress increased monotonically; (2) the compressive stress initially decreased before increasing for the upper layer and increased monotonically for the lower layer; (3) the tensile stress increased sharply for both the upper and lower layers; and (4) both the tensile and compressive stresses stabilized.

(a)

(b)

(c)

2.2.1. Phase 1

In Phase 1, the stress increased monotonically. The stress on the rebar was mainly impacted by the weight of the freshly poured concrete and increase in temperature. The concrete pouring released a large amount of hydration heat, which caused the internal temperature of the concrete to rise. The coefficients of thermal expansion for rebar and concrete are approximately and , respectively, which means that the former is more temperature-sensitive than the latter. Consider the case where concrete is not added to rebar, and let and be the elongations of the rebar and concrete, respectively, for every 1°C increase in temperature. If rebar is added into concrete, the same 1°C increase in temperature would cause the elongation of the rebar to be constrained by the concrete because the former is larger in magnitude than the latter. In this case, the actual elongation of the rebar () will be smaller than , while the elongation of the concrete () will be greater than . Hence, the rebar is compressed by , which results in compressive stress. Meanwhile, the concrete is elongated by , which results in tensile stress (Figure 4). This phase lasted for roughly 1–3 days. As the temperature increased (Figure 3(c)), the compressive stress on the rebar increased significantly. Figure 5 plots the stress on the rebar distributed horizontally along the tunnel on day 3. On this day, both the upper and lower layers of the rebar experienced compressive stress. This stress reached a maximum at the center of the inverted arch of the tunnel for the lower layer, but this phenomenon did not occur in the upper layer. This may be explained by the uneven distribution of the concrete weight and temperature stress.

2.2.2. Phase 2

In Phase 2, the compressive stress first decreased before increasing for the upper layer and increased monotonically for the lower layer. There were two main contributing factors: the temperature stress and pressure from the surrounding rock. In this phase, the internal temperature of the concrete began to decrease. Let and represent the compressions of the rebar and concrete, respectively, for every 1°C decrease in temperature prior to the rebar being placed in concrete. After the rebar is placed in the concrete, the compression of the former is constrained by the latter. This also causes the actual compression of the rebar () to be less than , so the rebar is impacted by the tensile stress generated by the concrete. This is equivalent to a tensile strain equal to acting on the rebar. The concrete is also affected by compressive stress generated from the rebar, which is equivalent to a compressive strain of (Figure 6). Hence, the compressive stress on the upper layer of the rebar decreased gradually. Although the compressive stress did not decrease for the lower layer, there was a reduction in its rate of increase. This was mainly caused by the increase in stress on the rebar generated by the surrounding rock while the fall in temperature reduced the compressive stress on the rebar. This indicates that the compressive stress from the surrounding rock had a greater effect than the temperature stress on the lower layer of the rebar.

The field data for the early phases revealed that the free swell ratio of the surrounding rock was greater than 50% (i.e., swelling rock). Groundwater seeped into the rock surrounding the tunnel through cracks, which caused the rock to expand. This compressed both the tunnel invert and unexpanded rock, which created cracks in the unexpanded rock for more groundwater to seep in. The unexpanded rock then absorbed this groundwater, which in turn compressed the tunnel invert and other unexpanded rock. This cycle continued, which caused the lift on the tunnel invert to gradually increase (Figure 7). This in turn created the trend of increasing compressive stress on the lower rebar layer. Phase 2 lasted roughly from day 3 to day 15. Figure 8 shows the stress on the rebar horizontally distributed along the tunnel on day 15. Compared to day 3, the compressive stress on the upper layer decreased significantly while that on the lower layer increased somewhat to a maximum of 18.3 MPa. The compressive stress remained greatest at the center of the tunnel invert, which was mainly due to the expansion of swelling rock caused by groundwater seepage.

2.2.3. Phase 3

In Phase 3, the tensile stress increased sharply for both the upper and lower layers. The data showed that sustained rainfall (>12 h) occurred on day 42. The surrounding rock expanded sharply because of the large amount of rainwater seepage, which rapidly increased the lift on the tunnel invert (Figure 9). This compressed the lower part of the invert and stretched the upper part. This increased the compressive stress on the upper rebar and the tensile stress on the lower rebar. Figure 10 plots the stresses on rebar distributed horizontally across the tunnel on day 45. The tensile stress on the upper layer was the greatest at the center of the invert (13.8 MPa). Similarly, the compressive stress on the lower layer was the greatest at the same location (55.4 MPa) and was roughly 300% greater than the 18.3 MPa observed on day 15. Two to six days after the rain (i.e., days 43–47), the maximum compressive stress on the lower rebar of the invert increased from 35.7 MPa to 106.5 MPa. The stress on the upper rebar changed from a compressive stress of 2 MPa to a tensile stress of 17.3 MPa. In 5 days, the compressive stress increased threefold, and the tensile stress increased 9.5-fold. This indicates that the expansion of the surrounding rock was the main reason for the change in stress on the rebar.

Because of the rapid increase in tensile stress on the rebar, the tensile stress exceeded the tensile strength of the concrete, and cracks began to appear in the concrete. For sections where cracks appeared, the concrete withdrew from tension work, which was transferred to the rebar. This significantly increased the tensile stress. At locations away from the crack, the stresses on the rebar and concrete were redistributed. The stress on the rebar gradually decreased, and the stress on the concrete gradually increased to the tensile strength. When the load increased, secondary cracks appeared at other weak points. As the load increased, new cracks appeared until the structure was damaged.

2.2.4. Phase 4

In Phase 4, the stresses generated by the surrounding rock and groundwater had become stable, and the drag of the invert and external lift had roughly evened out. This caused the compressive and tensile stresses acting on the rebar to stabilize. Figure 11 plots the forces acting on the upper and lower layers of the rebar distributed horizontally along the tunnel. The compressive stress on the lower layer was the greatest at the center of the invert structure at roughly 119.7 MPa. This is a 12.4% increase over the stress on day 47 (roughly 106.5 MPa). Curve fitting showed that the stress on the rebar followed a Gaussian distribution. Table 1 presents the curve fitting formulas.

3. Discussion

The field data revealed that the process by which the rebar of a tunnel invert experiences stress is extremely complex and can be divided into four phases. In Phase 1, the stress on both the upper and lower layers of the rebar increased because of the concrete weight and increase in temperature from the hydration heat released during concrete pouring. When the concrete was poured, its weight acted directly on the rebar. This forced the rebar to settle vertically and compressed the upper and lower layers. After the concrete was poured, a large amount of hydration heat was released, and the concrete and rebar expanded thermally. However, the larger expansion coefficient of steel meant that the elongation of the rebar was constrained by its bond with the concrete, which placed the rebar under compressive stress. In Phase 2, the temperature began to decrease, and groundwater gradually converges towards the bottom of the tunnel, causing the surrounding rock to expand and the stress from the surrounding rock gradually increased. The temperature and surrounding rock had counteracting effects on the stress on the rebar. On the one hand, the hydration heat of the concrete was basically released, so the internal temperature of the concrete began to decrease. The bond between the rebar and concrete reduced the shrinkage of the rebar and caused it to be stretched, so the compressive stress on the rebar was reduced. On the other hand, the concrete realized certain strength and could resist part of the stress from the surrounding rock. Groundwater enters the bottom of the tunnel invert through seepage, causing the swelling rock at the bottom to absorb water and expand, and the expansion force directly acts on the tunnel lining structure; this helped increase the stress on the rebar. In Phase 3, the surrounding rock expanded mainly as a result of increased groundwater from continuous rainfall. The swelling of the surrounding rock expanded cracks that let more groundwater in. This sharply increased the lift acting on the invert and made it into a single-span statically indeterminate structure. This increased both the tensile stress acting on the upper layer of the rebar and the compressive stress acting on the lower layer of the rebar at the center of the invert. In Phase 4, the stresses from both the surrounding rock and temperature were largely stable. Because it was winter, the internal temperature of the concrete gradually decreased. However, the temperature decrease was limited, and the resulting temperature stress was negligible compared to the stress from the surrounding rock at this time. Therefore, the stress on the rebar gradually stabilized. This process is shown in Figure 12. Based on the four observed phases, the changes in the forces acting on the tunnel invert were deduced. This can be used to develop different measures for treating floor heave according to the phase, rather than according to the maximum stress. This will allow the floor heave of a tunnel invert to be controlled more accurately.

4. Conclusion

Field tests were performed to obtain the process by which stress acts on the rebar of an enriched water tunnel invert. This will provide data and theoretical support for the rational treatment of floor heave of enriched water tunnel invert. The main conclusions are as follows: (1)The stress on the rebar in a tunnel invert is extremely complex and can be divided into four major phases: (1) the stress increases monotonically; (2) the compressive stress initially decreases before increasing for the upper layer of the rebar and increases monotonically for the lower layer; (3) the tensile stress increases sharply for both the upper and lower layers; and (4) both the tensile and compressive stresses stabilize(2)After rainfall, a large amount of groundwater is replenished, and the swelling rock absorbs water and expands; the tensile stress on the upper layer of the rebar was the greatest at the center of the invert with a maximum value of roughly 17.3 MPa. The stress on the lower layer generally increased continuously over time. The compressive stress was the greatest at the center of the invert with a maximum value of roughly 120 MPa(3)The stress on the rebar in the tunnel invert is mainly related to two factors: the temperature and groundwater. As the temperature of the concrete increased and decreased, the differing expansion coefficients of concrete and steel and the bond with the concrete compressed or elongated the rebar. Groundwater determines the swelling force of swelling rock, and stress from the rock acted on the concrete of the invert, which was equivalent to a statically indeterminate structure under the jacking force. This damaged the invert by bending; the upper layer of the rebar was under tensile stress, while the lower layer was under compressive stress(4)Major changes in the stress on the rebar were observed 2–6 days after rain. The maximum compressive stress on the lower rebar increased from 35.7 MPa to 106.5 MPa, and the stress on the upper rebar changed from a compressive stress of 2 MPa to a tensile stress of 17.3 MPa. In 5 days, the compressive stress increased threefold, and the tensile stress increased 9.5-fold. This indicates that the expansion of surrounding rock caused by groundwater replenishment was the main reason for the change in stress on the rebar for Fuchuan Tunnel(5)The stresses on the upper and lower layers of rebar in the tunnel invert followed a Gaussian distribution after the forces stabilized

Data Availability

The data used to support the findings of this study are available from the corresponding author upon request.

Conflicts of Interest

The authors have no conflicts of interest to declare.

Acknowledgments

This work was supported by a Project of Shandong Province Higher Educational Science and Technology Program (No. J18KA194), Open Research Fund of Key Laboratory of Urban Underground Engineering of Ministry of Education (TUE2019-03), and National Key R&D Program of China (2018YFC1505300-2).

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Copyright © 2021 Mingqing Du et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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