1. Introduction
The excavation of a shallow buried loess tunnel causes changes and adjustments of the stress state of the overlying stratum in varying degrees. The construction deformation forms longitudinal cracks on the ground surface on both sides of the tunnel centerline in a short time. The cracks incline to the centerline line of the tunnel in the form of a curved surface in the depth direction and form a settlement grooves within a specific range of the stratum [
1,
2]. The soil in the groove is wedge-shaped and tends to slide toward the excavation free surface. When the tensile or shear stress of the slide trend surface is greater than the soil strength, the actual surrounding rock slide surface of the shallow loess tunnel forms [
3]. The slide surface is the most critical feature of the shallow buried loess tunnel, which provides a fast channel for the surface water infiltration [
4], and the deepest slip surface can reach near the tunnel lining. The water immersion softens the loess around the slide surface, resulting in the mechanical property decays rapidly with the increase of the sinking tendency of sliding wedge, which may cause the loads on the support structure and the deformation to increase. In severe cases, the secondary lining may crack and fall off [
5]. The flooding of the slide surface is bound to have a significant impact on the appearance and development of cracks.
The slide surface is significant in the calculation of the surrounding rock pressure of a shallow buried tunnel. It is generally believed that the weight of the subsidence soil inside the slide surface is the primary source of the surrounding rock pressure. K. Terzaghi believes that the combined force of the self-weight of the largest block EFGH inside the slide surfaces AB and CD, and the friction force on the EF and HG are the vertical surrounding rock pressure [
6], as shown in
Figure 1a. A. Bierbaumer believes that the vertical surrounding rock pressure is the combined force of the self-weight of the overlying block E’F’G’H’ and the friction in the E’F’ and G’H’ [
7], as shown in
Figure 1b. The weight and resistance of the subsidence soil determine the pressure of the surrounding rock. The shape and position of the slide surface determine the size of the subsidence soil and the resistance.
The uneven settlement of the overlying stratum of the tunnel is the root cause of the slide surface. Different engineering properties of loess, construction methods, and topographical features will lead to different deformation characteristics and laws [
8]. The corresponding slide surface will be different. The type of slide surfaces in previous studies did not consider the influence of the construction methods and the topographical features. The first purpose of this paper is to propose new types of slide surfaces that are suitable for shallow buried loess tunnels, considering the influence of the construction methods and topographic features.
The strength of the flooded loess decreases significantly, and the water is the most common cause of the large deformation and the cracking of the lining. The field monitoring results show that when the water content of Q2 loess stratum increases from 16.6% to 20.5%, the settlement rate of tunnel arch increases by 9.6 times [
9], and the surrounding rock pressure as well as the secondary lining pressure of the arch increase sharply. The lining cracks are mainly distributed in the arch and the sidewall. The arch cracking is the most serious, which precedes the sidewall [
10].
Research has been carried out on the influence of water immersion of surrounding rock on the lining structure of loess tunnels. For the collapsible loess tunnels, the vertical settlement of the lining caused by the rise of the groundwater level is higher than what caused by surface water infiltration without considering the slide surface [
11]. When the deformation of the loess tunnel foundation increases after immersion, the tensile stress of the vault in the flooded section decreases, and the pressure stress of the sidewall increases significantly near the flooded section [
12]. During the surface water infiltration process, the base pressure of the arch foot increases, whose settlement develops. The arch shoulder and the arch waist of the secondary lining are under compression, and the vault is under tension [
13]. The previous research about loess tunnel immersion mainly focused on immersion of surface and foundation without considering the slide surface as a transport channel and storage place for surface water. No research has been conducted on the effect of slide surface infiltration on shallow buried loess tunnels.
Cracking of tunnel lining is a common phenomenon, of which 80% are caused by deformation, the rest are caused by loads [
14]. The existing research about lining crack mainly involves two methods. One method is filed investigation with mathematical statistics to analyze the lining cracks, which reveals the distribution characteristics and laws of cracks as well as analyze the cracking grade and lining damage degree [
15,
16]. However, the test elements of the internal tunnel lining are prone to failure and cannot be monitored for a long time [
17]. The field investigation of cracks is only a result analysis of the lining cracking, which is usually regarded as evaluation means of work performance. The other method is the numerical simulation, with which most research about causes of lining cracking is obtained [
18]. Due to the limitation of the material constitution and other factors, it is difficult to research the entire process from lining cracking to lining instability with numerical methods. In contrast, the physical model test method can realize the whole process simulation of lining cracking and can provide the internal force and deformation of the lining at different cracking stages in detail. The second purpose of this paper is to study the cracking process and characteristics of the secondary lining with a physical model test, considering the immersion effect of the slide surface.
The paper proposes four types of slide surface of shallow buried loess tunnel, considering the influence of construction methods and stratum bias pressure. The immersion effect of the slide surface was simulated by applying the existing lining load to the lining model, and the value of the existing load on secondary lining caused by slide surface immersion was acquired by published studies [
19]. Finally, a secondary lining loading model test with a geometric similarity ratio of 1:10 was carried out to analyze the development of lining cracks and the corresponding changes in the internal force. What is more, the morphology of the lining crack in the thickness direction and the bearing capacity of the cracked lining were also analyzed.
7. Conclusions
The slide surface of the shallow buried loess tunnel may diagonally develop from the surrounding rock near the arch foot or the arch waist to the ground surface. Under the bias of stratum, the slide surface only exists on one side of the tunnel. The slide surface is a channel for water infiltration. Surface water can quickly infiltrate to the lining periphery through the slide surface, resulting in the deterioration of the mechanical property of loess as well as the deformation and cracking of the lining structure in varying degrees. Based on the above background, the effect of water immersion of different slide surfaces is simulated with the change of lining load. The cracking characteristics and internal force of secondary lining are studied in detail with a multi-point independent loading test system for tunnel lining. The main conclusions are as follows.
(1) The type of slide surface of the shallow buried loess tunnel is closely related to tunnel excavation methods and stratum bias. The failure point of surrounding rock around the tunnel may be located at the arch foot or arch waist, the shape of the slide surface is an oblique straight line, and the sliding surface only exists on one side of the tunnel under the biased stratum. Four types of slide surfaces of shallow buried loess tunnel are proposed.
(2) The immersion of the slide surface has the most significant effect on the deformation of the lining vault and arch waist. The cracking of the arch foot and the inverted arch has no apparent effect on the lining deformation, while the cracking of the vault and arch waist may change the lining deformation rate. The lining cracks are symmetrically distributed under the immersion of the bilateral slide surface, and the cracks are concentrated on the immersion side of the unilateral slide surface. The appearance of compressive cracks can be regarded as a precursor of lining instability.
(3) In the bilateral slide surface immersion cases, the axial force of the lining arch always increases with fluctuating bending moment, whose cracking affects the change rate of the internal force. In unilateral slide surface immersion cases, when the failure point is the arch foot, the axial force of the lower section of the sidewall is higher than that of the upper section. When the failure point is the arch waist, the axial force of the lower section of the sidewall is smaller than that of the upper section. The lining bending moment of the unilateral slide surface immersion is significantly higher than that of the bilateral slide surface immersion.
(4) In the thickness direction, lining cracks will always begin to develop with I-type initial cracks, then develop into L-type medium-term cracks, and finally develop into Y-type late-term cracks. The proportion of cracks in the medium-term is relatively large, and the initial and late-term cracks account for a relatively small proportion.
(5) After the lining has cracked for the first time, the cracked linings under different slide surface immersion cases that can continue to bear the load ratio are all less than 40%. With the increase of cracks, the allowable load ratio of cracked lining decreases linearly. Among them, the allowable load ratio under unilateral arch waist slide surface immersion cases decayed fastest, and the decay rate of allowable load ratio under the other three slide surface immersion cases was basically the same.