Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
-
Jianyong Han
, Yongzhong Zhang
Abstract
A high geo-stress environment severely damages tunnel structures owing to the large deformation of the surrounding rock, thereby threatening their safety. In this study, the Wushaoling highway tunnel group, which passes through a high geo-stress environment, is investigated as a case study. The spatial distribution of different types of tunnel cracks is analyzed based on the site observations. The lining crack variations, such as circumferential and longitudinal cracks, with the factors including grade of the surrounding rock, location of buried depth, and design type of the tunnel lining are investigated. Various structural reinforcement technologies are presented based on the damage degrees of the tunnel linings. Several finite element models of supporting structures are established to reveal the mechanism of tunnel crack control technology. The results show that longitudinal and circumferential cracks are the main characteristics of tunnel lining damage in high geo-stress environments, accounting for approximately 29.4 and 53.2% of the total cracks, respectively. SIVb-, SVc-, and SVd-type linings show numerous longitudinal cracks per kilometer. The longitudinal cracks appear primarily on the tunnel crown and hance. In terms of the lining support types in Grade V surrounding rocks, the number of longitudinal cracks per kilometer increases with the lining grade. The number of tunnel cracks per kilometer tends to increase with the buried depth. Four tunnel structure reinforcement treatment measurements for lining cracks in high geo-stress condition were innovatively proposed, which were proved effective in deformation controlling and strengthening the tunnel lining using numerical investigation. The key contribution of this research is to reveal the characteristics and evolution mechanism of tunnel lining cracks in high geo-stress condition, and provide effective treatments for the tunnel lining cracks. In addition, the findings from the study on the tunnel lining cracks also provide industry practitioners with a comprehensive guide regarding the characteristics and control techniques of the tunnel lining cracks, which can serve as a steppingstone to facilitate the construction technology development of the transportation industry.
1 Introduction
Owing to continuous economic and social developments, the scale and number of transportation and engineering projects are steadily increasing. As an underground traffic structure, a tunnel becomes longer, larger, deeper, and more difficult to construct [1] after it has entered the rapid-development phase [2]. Therefore, the tunnel construction process is typically affected by complex geological conditions such as high water pressure, high permeability, high geo-stress, and low stratum bearing capacity. Among them, high geo-stresses in soft rock strata are particularly difficult to overcome. The weak surrounding rock, which is characterized by its low strength features such as softness, weakness, looseness, and fragmentation, has an extremely low load-bearing capacity. For tunnels with high geo-stress owing to significant depths or complex structural stresses, the surrounding rock mass is subjected to squeezing and tensile cracking due to the high geo-stress after excavation. This causes loosening and creep in the rock, thus resulting in numerous problems such as rock bursts and large deformations [3,4]. Over the long term after the completion of tunnel construction, various types of structural damage will occur, thereby affecting the normal usage and functionality of the tunnel [5,6,7]. Therefore, one must examine the characteristics of soft rock tunnel structural damage in high geo-stress environments and develop a comprehensive set of control techniques for tunnel lining cracks under high geo-stress.
Tunnel engineering worldwide is currently progressing deeper underground, where geological and geo-stress conditions are complex and variable. Many researchers have investigated the characteristics and mechanisms of large deformation in tunnels under high geo-stress conditions [8,9,10]. Zhao et al. [11,12] made outstanding achievements in the study of large deformation in tunnels. Taking the Haba Snow Mountain Tunnel as a case study, they studied the evolution of high geo-stress in tunnels based on field monitoring. Furthermore, a prediction method for large deformation in high geo-stress tunnels was proposed. They also innovatively introduced an advanced stress-release technology for super-deep soft-rock tunnels. Large deformation in tunnels often leads to significant structural damage and failure. Jiang et al. [13] measured and analyzed the temporal evolution of the tunnel large deformation in high geo-stress conditions, and presented an advanced measure technology based on a 3D laser scanner and processing algorithm for point cloud data. Thus, large-scale tunnel structural damage caused by large deformations in high geo-stress environments has garnered considerable research interest [14,15,16,17]. Dai et al. [18] classified tunnel damage by categorizing cracks into three types: circumferential, longitudinal, and inclined cracks. Focusing on a water-rich soft rock roadway in the Wangzhuang coal mine, Xue et al. [19] identified severe stress concentration in the roof and floor of the tunnel, which resulted in continuous cracking, rock damage, reduced strength, and stress release. Wang [20] identified extensive deformation of the surrounding rocks in various sections of the Xuecheng tunnel during its operational period, including severe longitudinal cracking and significant inclined and transverse cracking of the sidewalls in certain sections. Based on the aforementioned findings, researchers have investigated the causes and influencing factors of tunnel structural damage. Zhao et al. [21] explored the reasons for tunnel structure failure according to on-site measurements. The results indicate that the first-layer support in the tunnel is damaged by the creep load from the surrounding rock. Chuang et al. [22] evaluated the constraint effect of supporting structures and the boundary effects of a three-dimensional model using the confinement convergence method. Bian et al. [23] integrated practical engineering with laboratory microanalysis and hypothesized that deformation in the Huangjiazhai tunnel was caused by plastic flow arising from tunnel excavation under high geo-stress and low rock strengths, in addition to a hydrated-mechanical coupling process between shales and water. In summary, tunnel structural damage has been primarily investigated by conducting field surveys, numerical simulations, or theoretical analyses, with particular emphasis on the characteristics and causes. However, most field studies focus on the field construction period of operation. Statistical analyses of tunnel structural damage during long-term operational processes are limited.
In previous studies pertaining to disaster control in high geo-stress tunnels, control support methods have been primarily categorized into flexible support and rigid support. Zhao et al. [24] proposed an advanced support system that combines yielding, resistance, and coordinated load-bearing, a stress control and release strategy for advanced lead holes in high geo-stress tunnels based on the dynamic evolution mechanism of the surrounding rock. To mitigate the large deformation of surrounding rocks in soft-rock tunnels, Liu [25] introduced a dynamic design method for twin main supports using energy conversion theory. Chen et al. [26] adopted single and double primary support methods successively. The results revealed that the double primary support method effectively controlled the large deformation and rheological effects of broken phyllite under high geo-stress. Li et al. [27] discovered that the combination of long and short anchor rods intersecting at large angles with rock layers, combined with grouting, effectively strengthened the surrounding soft rock. Using the finite element method, Xu et al. [28] analyzed the mechanical characteristics of a corrugated steel plate supporting structure and evaluated the safety of the prefabricated supporting structure, which indicated that the corrugated steel plate possessed sufficient strength to restrain the deformation of the surrounding rock. Miao et al. [29] discovered that CRLD anchor support offered several advantages in rock-burst control, such as more uniform stress distribution in the surrounding rock, a uniform distribution of plastic zones, less prominent damage to the tunnel, and effective control of the arch top displacement. Tao et al. [30] evaluated the damage characteristics of surrounding rocks in the Muzhailing high geo-stress tunnel and presented a coupled support system of “negative Poisson’s ratio (NPR) anchor cable + steel arch frame + concrete” coupled support system. Focusing on a defective tunnel with a 60° arch crown in class III surrounding rocks, He et al. [31] investigated the effect of the stiffness of different internal surface reinforcement materials and ranges of the bearing capacity of the structure. Zhang et al. [32] proposed a novel energy absorbing material composed of foamed concrete-filled polyethylene pipe, which can be used as a high geo-stress soft rock tunnel. Wei and Zhou [33] applied reinforcement measures such as epoxy mortar grouting and inverted arch truss strengthening. However, the characteristics of tunnel structural damage under high geo-stress conditions have not been systematically examined in previous studies. Instead, control measures have only been proposed based on individual lining damage cases. Additionally, no comprehensive technical approach has been devised for alleviating tunnel lining damage in soft rock tunnels under high geo-stress environments by considering the characteristics of tunnel structural damage.
Thus, a case study of the Wushaoling highway tunnel group is conducted in this study based on long-term observations of tunnel lining crack characteristics under high geo-stress conditions. The abovementioned characteristics are analyzed by performing inspections and tests in construction sites. The effects of lining cracks and key parameters on the Wushaoling tunnel group are investigated. A deformation control system and tunnel lining crack treatment strategies for deeply buried soft rock tunnels under high geo-stress conditions are proposed and developed. Various treatments for tunnel cracks and structural damage are proposed, which yielded favorable control and reinforcement results. This study provides engineering application value for guiding tunnel lining crack management.
2 Project background
2.1 Project overview
The Wushaoling tunnel group is located in Gansu Province, China, at the convergence of the Loess, Inner Mongolian, and Qinghai-Tibet Plateaus, with an average elevation of approximately 2,400 m. This tunnel group comprises five tunnels: Wushaoling Tunnel (Wushaoling Tunnel 1#), Anyuan Tunnel (Wushaoling Tunnel 2#), Fuerwan Tunnel (Wushaoling Tunnel 3#), Gaoling Tunnel (Wushaoling Tunnel 4#), and Gulang Tunnel (Wushaoling Tunnel 5#). The total length of the tunnel group is 21.9 km. The maximum burial depth of the tunnels is 470 m. An illustration of the Wushaoling tunnel group is shown in Figure 1.

Illustration of the Wushaoling tunnel group.
Based on the terrain and geological conditions, the tunnels were designed as a separated layout. Each single tunnel is a two-lane tunnel, with a spacing of 42 m between the two single tunnels according to the Chinese code “Code for Design of Road Tunnel JTG D70-2004” [34]. The design speed of the tunnel is 80 km/h. The Wushaoling tunnel group includes four cross-sectional types based on the profile dimensions: standard section, emergency parking bay section, vehicular tunnel section, and pedestrian tunnel section. The standard tunnel section and emergency parking bay section are designed according to “Code for Design of Road Tunnel JTG D70-2004” [34] for a design speed of 80 km/h. The crown of the standard tunnel section adopts a single-circle semicircular arch with a radius of 5.43 m, while the side walls adopt an arc with a radius of 7.93 m (Figure 2). The building clearance width and height are 10.25 and 5 m, respectively. The crown of the emergency parking bay section adopts an arc with a radius of 7.37 m, the side arch adopts a radius of 7.93 m, and the side walls adopt an arc with a radius of 7.93 m. The invert radius is 18 m, and the connection between the invert and side walls uses a small-radius arc with a radius of 1.5 m. The building clearance width and height of the emergency parking bay section are 13 and 5.0 m. The vehicular tunnel section is designed using a triple-circle curved wall lining, having a building clearance width of 4 m and height of 5 m. The pedestrian tunnel section is designed using a single-circle straight wall lining, having a building clearance width of 2 m and height of 2.5 m.

Profile of tunnel lining cross-section of the Wushaoling tunnel group. (a) SIVb type. (b) SVb type. (c) SVI type.
A composite lining structure was used in the Wushaoling tunnel group. The principles of the new Austrian tunneling method were adopted during construction. Due to space limitations, only the typical profiles of the standard tunnel section are illustrated in Figure 2. Initial support is provided by combining shotcrete and metal mesh, and cast-in-place concrete is used in the secondary lining. The main materials used in the tunnel construction included C30 plain concrete and C35 reinforced concrete.
The design parameters for the composite lining of the Wushaoling tunnel group are listed in Table 1. A total of 22 types of tunnel sections have been designed in the Wushaoling tunnel group. The selection of the type of tunnel lining structure is based on factors such as the surrounding rock grade, tunnel depth, integrity of the surrounding rock, and cross-sectional dimensions. The lining type name corresponds to the tunnel section types and surrounding rock grade. The letters in the name of the tunnel lining represent the following aspects: S represents standard section, JS represents emergency parking bay section, TS represents intersection section, CS represents vehicular tunnel section, SR represents pedestrian tunnel section, the Roman number represents the grade of surrounding rock, and the letter at the end of the name represents different application conditions.
Parameters for composite lining of the Wushaoling tunnel group
Lining type | Surrounding rock grade | Initial support parameters | Secondary lining (cm) | Forepoling | ||
---|---|---|---|---|---|---|
Steel arch frame (cm/section) | Anchor rod (cm) | Steel mesh (cm) | ||||
SVI | VI | 50 (I20a) | 400/600 | 15 × 15 | 60 | R51L pipe roof |
SVa | V | 75 (I20a) | 350 | 15 × 15 | 50 | φ42/φ8 pipe roof |
SVb | V | 75 (I18) | 350 | 15 × 15 | 45 | φ42 forepoling steel pipe |
SVc | V | 75 (I20a) | 350 | 15 × 15 | 50 | φ42 forepoling steel pipe |
SVd | V | 75 (I20a) | 400 | 15 × 15 | 50 | φ89 pipe roof |
SVe | V | 75 (I20a) | 350 | 15 × 15 | 50 | R51L pipe roof |
SIVa | IV | 100 (16 × 16) | 300 | 20 × 20 | 40 | φ22 anchor rod |
SIVb | IV | 100 (18 × 18) | 300 | 20 × 20 | 40 | φ42 forepoling steel pipe |
SIVc | IV | 100 (I18) | 300 | 20 × 20 | 40 | φ42 forepoling steel pipe |
SIVd | IV | 100 (16 × 16) | 300 | 20 × 20 | 40 | |
SIII | II | 250 | 20 × 20 | 35 | φ42 forepoling steel pipe | |
JSV | V | 60 (I20a) | 350 | 15 × 15 | 45 | φ42 forepoling steel pipe |
JSIV | IV | 75 (18 × 18) | 350 | 20 × 20 | 40 | |
JSIII | III | 100 (18 × 18) | 300 | 20 × 20 | 40 | φ42 forepoling steel pipe |
TSV | V | 75 (I20a) | 400 | 15 × 15 | 60 | φ42 forepoling steel pipe |
TSIV | IV | 75 (I18) | 350 | 20 × 20 | 50 | |
TSIII | III | 100 (18 × 18) | 350 | 20 × 20 | 45 | |
CSV | V | 300 | 20 × 20 | 35 | ||
CSIV | IV | 300 | 20 × 20 | 35 | ||
CSIII | III | 250 | 20 × 20 | 30 | ||
SRa | V/IV | 250 | 20 × 20 | 30 | ||
SRb | III | 200 | 25 |
2.2 Geological and hydrogeological conditions
2.2.1 Geological conditions
The topography of the tunnel site area can be described as a mid-high mountain and valley region. The tunnel group is located in the Wushaoling fault-fold zone, which is characterized by a stable strip-like distribution in width. The tunnel group crosses several regional faults, including the Xiaganchaigou-Xindunwan thrust fault (F7), the Shanghuangcaochuan-Hongguangou thrust fault (F6), the Tianhewan thrust fault (F5), and the Miaoergou-Dalong Village North thrust fault (F4). The fault dip angles of these faults range from approximately 55° to 70°. Wushaoling Tunnel 1# has extremely developed fault structures.
According to geological exploration data, the surrounding rocks of the Wushaoling tunnel group are predominantly categorized as Grades V and IV, based on the rock classification regulations in the code “Standard for Engineering Classification of Rock Mass GB/T 50218-2014” [35], as presented in Table 2. Rock mass is primarily classified based on two factors: the qualitative characteristics and basic quality (BQ) of rock mass. Additionally, the modification effects of groundwater, structural planes, and the initial stress state on the BQ of rock mass must be considered. The detailed rock mass classification regulations are listed in Table 3.
Percentage of surrounding rock grades in the Wushaoling tunnel group
Tunnel name | Grade IV surrounding rock (m) | Grade V surrounding rock (m) | Total tunnel length (m) |
---|---|---|---|
Wushaoling Tunnel up-line | 2,040 (41.59%) | 2,865 (58.41%) | 4,905 |
Anyuan Tunnel up-line | 1,950 (28.39%) | 1,938 (28.22%) | 6,868 |
Anyuan Tunnel down-line | 1,990 (29.06%) | 1,898 (27.72%) | 6,848 |
Gaoling Tunnel up-line | 2,150 (33.95%) | 2493.4 (39.37%) | 6,333 |
Gaoling Tunnel down-line | 1,990 (31.52%) | 1,898 (30.06%) | 6314.45 |
Rock mass classification
Rock mass classification | Qualitative characteristics | BQ |
---|---|---|
Grade I | Hard rock and intact rock mass | >550 |
Grade II | Hard rock and relatively intact rock mass; relatively hard rock and intact rock mass | 550–451 |
Grade III | Hard rock and relatively fractured rock mass; relatively hard rock and relatively intact rock mass; relatively soft rock and intact rock mass | 450–351 |
Grade IV | Hard rock and fractured rock mass; relatively hard rock and relatively fractured to fractured rock mass; relatively soft rock and relatively intact to relatively fractured rock mass; soft rock and intact to relatively intact rock mass | 350–251 |
Grade V | Relatively soft rock and fractured rock mass; soft rock and relatively fractured to fractured rock mass; all extremely soft rock and all extremely fractured rock mass | ≤250 |
The lithologic composition of the tunnel through strata is complex and includes new loess, gravelly soil, cobble soil, pebble soil, sandstone, metamorphic sandstone, slate, phyllite, andesite, and mudstone. Figure 3 shows a cross-section profile of the geological layers intersected by the Wushaoling Tunnel. The multiple lithologic boundary interfaces cause significant changes to the rock phases, thus resulting in well-developed fractures. The integrity of the rock mass is extremely poor owing to the presence of faults and the high degree of weathering. Consequently, the surrounding rocks exhibit a limited self-stabilization capacity.

Cross-section profile of geological layers intersected by Wushaoling Tunnel.
To obtain the geo-stress condition of the Wushaoling tunnel group, geo-stress tests were conducted using the hydraulic fracturing method, which is essentially a two-dimensional method for measuring geo-stress. For the hydraulic fracturing method, high-pressure water was injected into a test section sealed by packers to induce hole wall fracturing. Subsequently, the magnitude and direction of the maximum and minimum principal stresses in the horizontal plane were determined based on the theories of elastic mechanics. The geo-stress test results of one of the boreholes for the Wushaoling tunnel group are presented in Table 4. The surrounding rock parameters obtained by drilling samples reveal that the maximum horizontal principal stress (σ H) around the tunnel generally ranged from 3.76 to 9.82 MPa, whereas the minimum horizontal principal stress (σ h) ranged from 2.48 to 3.74 MPa. A comparison of the magnitudes of the three principal stresses indicates that the current stress shows σ H > σ h > σ v (σ v, the vertical principal stress), thus indicating that the horizontal principal stress is the maximum and the vertical principal stress is the minimum. This suggests that tectonic stress dominates in the Wushaoling tunnel group. Based on measured geo-stress, the current σ H in the tunnel area lies along the NNE direction.
Results of geo-stress tests for the Wushaoling tunnel group
Serial number | Fracturing depth (m) | Fracturing parameters (MPa) | Stress value (MPa) | |||||||
---|---|---|---|---|---|---|---|---|---|---|
P b | P r | P S | P H | P 0 | T | σ H | σ h | σ v | ||
1 | 93.3–94.0 | 4.59 | 2.79 | 2.29 | 0.94 | 0.32 | 1.80 | 3.76 | 2.29 | 2.48 |
2 | 107.3–108.0 | 9.35 | 4.93 | 4.54 | 1.08 | 0.46 | 4.42 | 8.23 | 4.54 | 2.85 |
3 | 111.4–112.1 | 5.47 | 3.81 | 3.43 | 1.12 | 0.50 | 1.93 | 5.98 | 3.43 | 2.96 |
4 | 119.8–120.5 | 6.78 | 5.24 | 4.28 | 1.20 | 0.58 | 1.54 | 7.02 | 4.28 | 3.18 |
5 | 124.1–124.8 | 7.20 | 4.70 | 4.70 | 1.24 | 0.62 | 2.50 | 8.78 | 4.70 | 3.30 |
6 | 130.2–130.9 | 12.46 | 7.85 | 6.12 | 1.31 | 0.69 | 4.61 | 9.82 | 6.12 | 3.46 |
Note: P b is the initial fracturing pressure; P r is the re-fracturing pressure; P s is the instantaneous closure pressure; P H is the instantaneous closure pressure of pre-existing fractures; P 0 is the pore water pressure; T is the in situ tensile strength; σ H is the maximum horizontal principal stress; σ h is the minimum horizontal principal stress; σ v is the vertical principal stress.
The deep burial surrounding rock and stress characteristics of the tunnel are shown in Table 5. According to the code “Specifications for Design of Highway Tunnels JTG D70-2014” [36], when R c/σ max < 4, it is classified as extremely high geo-stress and 4 < R c/σ max < 7 is classified as high geo-stress. For σ max set at 9.82 MPa, the R c/σ max values are as indicated in Table 5. Clearly, in the Triassic system sandstone, mudstone interlayers, structural belt, and other soft and weak rock layers of the tunnel section, the areas were characterized by extremely high geo-stress zone, with clear rheological deformation characteristics observed in the surrounding rock, which is susceptible to severe tunnel deformation. In the Ordovician metamorphic sandstone and slate tunnel sections, where local zones were strongly sericitized and chloritized with phyllite characteristics, the rock was soft and weak, with some sections belonging to high geo-stress areas, and the surrounding rock was primarily characterized by rheological deformation. In the Ordovician andesite basalt tunnel section, the R c/σ max ranged between 4 and 7, with local peeling and block dropping possible.
Stability of surrounding rock and stress characteristics of the tunnel
Serial number | Geological era | Rock mass designation | Rock mass characteristics | Statement | Hardness level (MPa) | R c/σ max | Surrounding rock stability |
---|---|---|---|---|---|---|---|
1 | Tn | Interbedded sandstone and mudstone | Light red, medium to coarse-grained structure conglomeratic structure, stratified structure | Soft rock | 0.5–5 | 0.05–0.51 | Primarily characterized by rheological deformation |
3 | Oz | Metamorphic sandstone slate | Light gray to gray-green, medium to coarse-grained structure, stratified structure | Relative hard rock | 40.6–89.4 | 4.13–9.10 | Rheological deformation in localized sections |
4 | Oz | Andesite basalt | Flesh red, mottled structure, with pores or almond-shaped structures | Hard rock | 62.9 | 6.41 | Peeling and block dropping occurred |
Note: R c is the uniaxial saturated compressive strength of rock; σ max is the maximum initial stress in the direction perpendicular to the tunnel axis.
2.2.2 Hydrogeological conditions
The tunnel site area is within the hydrogeological zone of the eastern segment of the Qilian Mountains. The groundwater of the tunnel site can be categorized into two types: Quaternary loose pore water and bedrock fracture water. The former is discovered in the Quaternary cover layers and gravel-pebble layers at the tunnel entrances, whereas the latter is distributed in structural fractures within the bedrock and extensively developed superficial networked weathered fractures. Both groundwater types are replenished by atmospheric precipitation. The annual average precipitation in the tunnel site area is approximately 400 mm. A simple analysis of the groundwater samples obtained from the tunnel site area revealed that the pH ranges from 7.94 to 8.23 and that corrosive CO2 does not exist. The Wushaoling mountain primarily comprises detrital rocks with extensive weathered and structural fractures. Although the high-altitude bedrock of the mountain receives abundant rainfall and has ample water supply, the presence of deep valleys and the development of surface hydrological networks typically cause groundwater to depart from the fissures, migrate downslope, and discharge into the valleys.
3 Tunnel structural damage characteristics under high geo-stress conditions
The tunnel lining cracks are direct manifestation of structural damage in tunnels. The tunnel lining cracks are closely related to large deformation disasters, especially under conditions of high geo-stress and soft surrounding rock. The tunnel lining cracks and large deformation disasters often coexist or induce each other.
The Wushaoling highway tunnel investigated in this study and the existing Wushaoling railway tunnel are both located in Wushaoling Mountains in Gansu Province, China. Although they are situated in different parts of the mountain range, the two tunnels are roughly parallel and close to each other with a distance of a few hundred meters to several kilometers, each traversing through the mountainous terrain. The existing Wushaoling railway tunnel, built between 2003 and 2006, has been confirmed to exhibit significant large deformation of the surrounding rock due to the influence of high geo-stress [37,38,39,40]. Therefore, the Wushaoling highway tunnel and the existing railway tunnel share similar geological conditions in the strata they traverse.
The Wushaoling highway tunnel group was built between 2009 and 2013, and due to its considerable burial depth, high geo-stress, soft surrounding rock, and fault fracture zones in the strata resulted in significant large deformation of the surrounding rock during construction and operation. The large deformation of the surrounding rock imposes considerable stress on the tunnel lining, causing structural cracking in the lining due to insufficient bearing capacity [24]. Additionally, after tunnel excavation, the release of stress and the creep effect in the surrounding rock persist for an extended period. The stress on the tunnel lining structure gradually increases, resulting in delayed cracking.
During the 8 years of operation since the tunnel completion, the Wushaoling tunnel group experienced numerous deterioration issues such as lining cracks, water leakage, and pavement uplift. This study focuses on the statistical analysis of tunnel lining crack characteristics under high geo-stress conditions. Due to limited site access and maintenance funds, a systematic investigation of the large deformation pattern of the surrounding rock in the Wushaoling highway tunnel was not conducted. Nevertheless, a detailed discussion of the distributions of cracks in the Wushaoling tunnel group over 3 years was provided. Meanwhile, the impact of surrounding rock conditions, lining types, and tunnel depth on lining cracks was investigated. Based on these analyses, the mechanisms of tunnel lining crack formation under high geo-stress conditions were revealed, and suitable control technologies for lining cracks in different sections were proposed.
Owing to favorable geological conditions, the Fuerwan Tunnel and Gulang Tunnel within the Wushaoling tunnel group do not exhibit prominent lining damage features. Therefore, the case studies were primarily based on field observations of the Wushaoling Tunnel, Anyuan Tunnel, and Gaoling Tunnel.
3.1 Types of structural cracks in tunnel lining
Under high geo-stress conditions, significant deformation typically occurs in tunnel linings, accompanied by severe cracking of the lining structure. The generation and development of structural cracks in the tunnel lining can jeopardize tunnel structural safety and, in severe cases, affect the safe operation of the entire tunnel. To assess the hazard of cracking in tunnel lining structures, the common classifications and crack characteristics should be evaluated comprehensively.
Based on the relationship between crack orientation and the longitudinal axis of the tunnel, structural cracks in tunnel linings can be classified into longitudinal, inclined, circumferential and closed cracks. The measured tunnel lining cracks are shown in Figure 4.

Measured structural cracks in the tunnel lining (taken by a tunnel lining crack detection vehicle).
3.1.1 Longitudinal cracks
Cracks that are almost parallel to the longitudinal axis of the tunnel are referred to as longitudinal cracks. These longitudinal cracks are primarily caused by compressive forces on the inner edge of the arch crown and tunnel hance, which results in the squeezing, cracking, and block detachment of the inner concrete lining. Among the different types of cracks, longitudinal cracks pose the highest risk to tunnel structural safety. They can cause minor issues such as arch crown collapse or more severe consequences such as the collapse of the entire tunnel.
3.1.2 Inclined cracks
Inclined cracks are orientated at approximately 45° to the tunnel axis and occur in both the sidewalls and arch section. They typically emerge due to a combination of longitudinal and circumferential forces exerting on the tunnel lining structure. Although inclined cracks are generally less hazardous than longitudinal cracks, they are more problematic than circumferential cracks. Thus, caution should be exercised when focusing on areas where multiple inclined cracks intersect during tunnel damage treatment. This is because the intersection of multiple inclined cracks generally results in the detachment of lining blocks.
3.1.3 Circumferential cracks
Circumferential cracks are almost perpendicular to the tunnel axis. They often occur owing to the uneven settling of the structure and are primarily observed at the junction of intact rock strata and unfavorable geological zones or construction and deformation joints. Compared with the other two crack types, circumferential cracks are less hazardous.
3.1.4 Closed cracks
Closed cracks typically exhibit a form similar to a grid or network and are distributed in a continuous, dense, and relatively regular manner. This type of crack, particularly in the surrounding rock, results in an uneven stress distribution, which exerts higher stresses in the local area of the tunnel lining and causes significant deformation to the surrounding rock mass.
3.2 Statistical analysis of tunnel lining cracks in the Wushaoling tunnel group
Based on the recognition and analysis of the tunnel internal contour photographs captured by a tunnel lining crack detection vehicle, the statistical results for the lining cracks of the Wushaoling Tunnel, Anyuan Tunnel, and Gaoling Tunnel of the Wushaoling Tunnel group were analyzed. A total of 4,974 circumferential cracks were discovered in the tunnel lining concrete, with a combined length of 16,816 m and a width ranging from 0.10 to 0.99 mm. Additionally, 2,747 longitudinal cracks, with a combined length of 9,610 m and a width between 0.10 and 0.99 mm were discovered. Furthermore, 1,484 inclined cracks were identified, with a combined length of 4,660 m and a width between 0.10 and 0.99 mm. Based on the crack inspection data obtained from the Wushaoling Tunnel, Anyuan Tunnel, and Gaoling Tunnel, the quantity and length of the tunnel lining cracks were analyzed (Figure 5). As shown in Figure 5, both the up-line and down-line tunnel linings exhibited numerous longitudinal and circumferential cracks. In the up-line, circumferential cracks dominated, i.e., constituting 54.7% of the total number of cracks and 52.8% of the total crack length. In the down-line, circumferential cracks account constituted 53.1% of the total number of cracks and 55.1% of the total crack length. Besides circumferential cracks, longitudinal cracks have the second-highest proportion, accounting for approximately 29.4% of the total number of cracks and 30.9% of the total crack length. By contrast, inclined cracks constitute a smaller proportion, ranging approximately from 13 to 17% of the total number of cracks in the Wushaoling tunnel lining, which is caused by the fault activity that the tunnel passes through.

Statistics on lining cracks in the Wushaoling tunnel group. (a) Up-line. (b) Down-line.
3.3 Analysis of lining cracks in Wushaoling tunnel group
This section presents the spatial distribution patterns of different crack types of cracks based on the analysis of crack inspection data from the Wushaoling Tunnel.
3.3.1 Characteristics of circumferential cracks
The up-line and downline tunnels of the Wushaoling Tunnel had 934 and 566 circumferential cracks, respectively. The stress of the surrounding rocks applied to the tunnel structure near the tunnel entrance differed significantly from that inside the tunnel. Thus, the number of circumferential cracks in the up-line and down-line within different distances from the tunnel entrance were analyzed, as shown in Figure 6.

Statistics on circumferential cracks in the tunnel lining of Wushaoling Tunnel. (a) Up-line. (b) Down-line.
As shown in Figure 6, the number of circumferential cracks in the up-line of the tunnel significantly exceeded that in the down-line. A total of 131 circumferential cracks were observed within the first 500 m from the tunnel entrance of the up-line. This can be attributed to the rock mass in this section, which comprised alluvial gravelly soil with a slightly cohesive silt texture and high clay content. The soil is susceptible to water loss and shrinkage deformation, and thus, the surrounding rocks must be closed promptly, and timely anchorage support must be provided after tunnel completion. The density of the circumferential cracks was the highest within 1,500–2,500 m from the tunnel entrance, which is primarily due to the geological conditions. In this area, the rock strata were of Grade IV, which comprised fragmented mudstone and carbonaceous shale and underwent deformation and damages phenomena such as rock fragmentation and block sliding/falling. Consequently, the lining deformed severely, and dense cracks emerged. The up-line section, which was beyond 2,500 m from the tunnel entrance, exhibited a balanced distribution of circumferential cracks. Meanwhile, the down-line section featured uniformly distributed circumferential cracks, with 40–50 cracks per 500 m. Dense circumferential cracks were only observed within a distance of approximately 500 m from the tunnel exit and 1,500–2,000 m from the tunnel entrance.
To further analyze the spatial distribution of circumferential cracks across the tunnel’s transverse section, the up-line was partitioned into three sections based on mileage to analyze the circumferential crack data. The resultant characteristics of the cross-sectional height distribution for circumferential cracks in the Wushaoling Tunnel are shown in Figure 7.

Characteristics of cross-sectional height distribution for circumferential cracks in Wushaoling Tunnel. (a) Within approximately 500 m from tunnel entrance. (b) Within approximately 1,000–1,500 m from tunnel entrance. (c) Within approximately 1,500–2,000 m from tunnel exit.
As shown in Figure 7, circumferential cracks occurred more frequently near the arch crown within the first 500 m from the tunnel entrance of the up-line, whereas fewer occurrences were observed near the sidewalls. The circumferential cracks were relatively uniformly distributed with respect to the height within 1,000–1,500 m from the tunnel entrance. Meanwhile, within 1,500–2,000 m from the tunnel entrance, the cracks were primarily concentrated near the sidewalls. In terms of the origin of the circumferential cracks, only the closed arch structure was able to withstand high pressures. If no invert exists or if construction quality of the inverted arch is low, then lining structure cannot effectively bear support pressure from the surrounding rock over the arch crown, thereby resulting in overall subsidence. When adjacent sections of the lining experience inconsistent overall settlement, circumferential cracking or even misalignment of the lining can occur.
3.3.2 Characteristics of longitudinal cracks
The up-line and down-line of the Wushaoling Tunnel had 846 and 667 longitudinal cracks, respectively. The number of longitudinal cracks in the up-line and down-line within different distances from the tunnel entrance was analyzed, as shown in Figure 8. The region with the highest number of longitudinal cracks in the up-line was 1,500–2,500 m from the tunnel entrance (369 cracks). In contrast, the down-line exhibited a uniform distribution of longitudinal cracks, with a higher number of longitudinal cracks appearing near the tunnel exit. Within a distance of approximately 500 m from the tunnel exit, 139 longitudinal cracks were observed. Areas with many longitudinal lining cracks exhibited concentration of circumferential cracks. Dense lining cracks were primarily due to severe lining deformation due to complex geological conditions.

Statistics on longitudinal cracks in tunnel lining of Wushaoling Tunnel. (a) Up-line. (b) Down-line.
To further analyze the spatial distribution of longitudinal cracks across the tunnel’s transverse section, the up-line was partitioned into three sections based on mileage, and the longitudinal crack data were analyzed. The resultant characteristics of the cross-sectional height distribution for longitudinal cracks in the Wushaoling Tunnel are shown in Figure 9. Within a distance of approximately 500 m from the tunnel entrance, longitudinal cracks did not exhibit a pronounced concentration in terms of height but appeared in greater quantity at the arch crown. However, within 1,500–2,000 m from the tunnel entrance, longitudinal cracks were primarily concentrated along the tunnel sidewalls, which corresponded to the region with more circumferential cracks. Moreover, longitudinal cracks tend to concentrate in the hance within 1,000–1,500 m from the tunnel exit and measured 5 m in height. Therefore, longitudinal cracks in the tunnel lining primarily occur near the tunnel crown and hance, which is consistent with the findings of the study conducted by Jiang et al. [13] on large deformation of the Jinchuan No. 2 Mine using 3D laser scanning.

Characteristics of cross-sectional height distribution for longitudinal cracks in Wushaoling Tunnel. (a) Within approximately 500 m from tunnel entrance. (b) Within approximately 1,000–1,500 m from tunnel exit. (c) Within approximately 1,500–2,000 m from tunnel entrance.
3.3.3 Characteristics of inclined cracks
The up-line and down-line of the Wushaoling Tunnel had 416 and 304 inclined cracks, respectively. The number of inclined cracks in the up-line and down-line within different distances from the tunnel entrance were analyzed, as shown in Figure 10. The region with the most inclined cracks in the up-line was within 2,000–2,500 m from the tunnel entrance (135 cracks). Meanwhile, the down-line had the most inclined cracks within 2,500–3,500 m from the tunnel entrance (142 cracks). Inclined cracks were primarily observed in the mid-section of the tunnel, with fewer instances near the tunnel entrance and exit.

Statistics on inclined cracks in the tunnel lining of Wushaoling Tunnel. (a) Up-line. (b) Down-line.
To further analyze the spatial distribution of inclined cracks across the tunnel’s transverse section, the up-line was partitioned into three sections based on mileage, and inclined crack data were sorted, as shown in Figure 11. Within 2,000–2,500 m from the tunnel entrance in the up-line, areas with the most inclined cracks were primarily along the tunnel sidewalls at a height of less than 2 m. Within a 3,000–3,500 m from the tunnel entrance in the down-line, inclined cracks were more prevalent near the tunnel arch crown.

Characteristics of cross-sectional height distribution for inclined cracks in Wushaoling Tunnel. (a) Within 2,000–2,500 m from the tunnel entrance. (b) Within 3,000–3,500 m from the tunnel exit.
3.3.4 Long-term development characteristics of tunnel lining cracks
Based on long-term monitoring of the Wushaoling Tunnel, the results of tunnel lining crack statistics from 2017 to 2019 were analyzed, as shown in Figure 12. The number of circumferential cracks decreased annually, which is primarily attributed to effective lining damage management. Meanwhile, the number of longitudinal cracks increased slightly in the down-line in 2018, although a decreasing trend was shown in general. By 2019, the number of longitudinal cracks in the down-line decreased to approximately 400. The increase in the number of longitudinal cracks and inclined cracks in 2018 is attributed to the continuous deformation caused by the creep characteristic of surrounding rock under the high geo-stress conditions and fault structures.

Annual comparison of tunnel lining crack status in Wushaoling Tunnel. (a) Circumferential cracks. (b) Longitudinal cracks. (c) Inclined cracks.
4 Tunnel lining cracks and influence patterns of key parameters
Based on the analysis of the technical assessment and inspection report of the Wushaoling tunnel group, the primary crack characteristics in the tunnel group, namely, circumferential and longitudinal cracks, were further investigated. The aim was to establish functional relationships between circumferential/longitudinal cracks and factors such as the surrounding rock grade, burial depth, and design type.
4.1 Relationship between tunnel lining cracks and surrounding rock grade
Tunnel lining cracks primarily result from the pressure and deformation exerted on the tunnel lining by the surrounding rocks. The lower the grade of the surrounding rock, the lower is the bearing capacity of the surrounding rock, and the higher the load bearable by the tunnel lining. Therefore, tunnel lining cracks are highly correlated with the grade of the surrounding rocks. Statistical analysis was conducted for longitudinal and circumferential cracks in the up-line and down-line of the Wushaoling Tunnel by considering different surrounding rock grades, as shown in Figure 13.

Relationship between surrounding rock grade and quantities of lining cracks in Wushaoling Tunnel. (a) Longitudinal cracks. (b) Circumferential cracks.
Both longitudinal and circumferential cracks were more prevalent in Grades IV and V surrounding rocks, which corresponded to the longer span of the surrounding rocks in the Wushaoling Tunnel, than in Grade VI surrounding rocks. Therefore, further analysis was conducted to determine the number of longitudinal and circumferential cracks per kilometer for different surrounding rock grades, as shown in Figure 14.

Quantities of longitudinal and circumferential cracks per kilometer in Wushaoling Tunnel. (a) Longitudinal cracks. (b) Circumferential cracks.
As shown in Figure 14, the highest number of longitudinal cracks per kilometer was observed in Grade IV surrounding rocks, i.e., approximately 220 cracks per kilometer, which surpassed those of the other two surrounding rock grades. This is primarily attributed to the non-consideration of the closure invert in the initial design for supporting Grade IV surrounding rocks, which resulted in unsatisfactory control over surrounding rock deformation. The Grade VI surrounding rocks had fewer circumferential cracks compared with the surrounding rocks of the other two grades. Despite the severe fragmentation of Grade VI surrounding rocks, the use of the SVI-type support structure controlled the deformation significantly.
4.2 Relationship between tunnel lining cracks and design type
In addition to the surrounding rock grade, tunnel lining cracks are directly related to the design type of the tunnel lining. Different lining cross-sectional structural types were designed for the Wushaoling Tunnel based on the surrounding rock grades. The relationship between the number of longitudinal/circumferential cracks and the tunnel lining design types was analyzed, as illustrated in Figure 15.

Relationship between design type and quantities of longitudinal and circumferential cracks in Wushaoling Tunnel. (a) Longitudinal cracks. (b) Circumferential cracks.
As shown in Figure 15, the SIVb- and SVb-type linings indicated the highest number of longitudinal cracks, i.e., 359 and 274 cracks, respectively, in the up-line. In the down-line, the SVb-type lining indicated the highest number of longitudinal cracks, i.e., 339 cracks. For the up-line, the SIVb- and SVb-type linings indicated the highest number of circumferential cracks, i.e., 323 and 362 cracks, respectively. In the down-line, the SIVb- and SVb-type linings indicated the highest number of circumferential cracks, i.e., 148 and 234 cracks, respectively. Thus, in both the up-line and down-line, the SIVb- and SVb-type linings indicated the highest numbers of longitudinal and circumferential cracks.
To compare the probability of longitudinal and circumferential cracks appearing in different lining types more effectively, the quantities of these cracks per kilometer for different lining design types were statistically analyzed, as shown in Figure 16.

Quantities of (a) longitudinal and (b) circumferential cracks per kilometer in Wushaoling Tunnel.
As shown in Figure 16a, the SIVb-, SVc-, and SVd-type linings indicated a high number of longitudinal cracks per kilometer. Additionally, the data indicate that as the tunnel lining grade increased for the Grade V surrounding rocks, the number of longitudinal cracks per kilometer increased as well. This is because, despite the continuous increase in the lining grade, the mechanical characteristics of the tunnel surrounding rocks deteriorated significantly, which resulted in the development of longitudinal cracks. For the tunnel section of the emergency parking strip, the TSIV-type lining structure was more susceptible to longitudinal cracks than the TSV-type lining structure. Fewer longitudinal cracks were observed in the open-cut section, primarily because the lateral pressure from the surrounding rocks was limited in this section and the load-bearing capacity of the lining was able to resist the lateral deformation of the surrounding rocks.
As shown in Figure 16b, in the up-line, the Grade IV and V surrounding rocks exhibited a similar density of circumferential cracks (i.e., 150–250 cracks per kilometer). However, fewer cracks were observed in the lining structures within the open-cut section, emergency parking strip, and fault zone. In the down-line, the SVc- and SVd-type linings exhibited the highest number of circumferential cracks (i.e., 329 and 257 cracks per kilometer, respectively).
4.3 Relationship between tunnel lining cracks and burial depth
In mountain tunnels, the geological structures typically exhibit considerable fluctuations in the ground surface above the tunnel. Different burial depths of the tunnel are typically associated with varying levels of surrounding rock pressure. Therefore, longitudinal cracks of different sections with different burial depths in the Wushaoling Tunnel were statistically analyzed. To eliminate the effects of factors such as the lining type and surrounding rock grade, a single-variable method was employed to evaluate the tunnel burial depth. As mentioned earlier, the SIVb- and SVb-type linings indicated a high number of longitudinal cracks. Therefore, a comparative analysis was conducted for the number of longitudinal and circumferential cracks in the SIVb- and SVb-type linings at different burial depths, as shown in Figures 17 and 18, respectively.

Relationship between the burial depth and quantity of longitudinal cracks in Wushaoling. (a) SIVb-type lining. (b) SVb-type lining.

Relationship between the burial depth and quantity of circumferential cracks in Wushaoling Tunnel. (a) SIVb-type lining. (b) SVb-type lining.
As shown in Figure 17, for the SIVb-type lining, the highest number of longitudinal cracks, i.e., 157 cracks, was observed at a burial depth of 130 m. For the SVb-type lining, the highest numbers of longitudinal cracks were observed at burial depths of 100 and 130 m, with 61 and 95 cracks, respectively.
As shown in Figure 18, for the SIVb-type lining, the highest numbers of circumferential cracks were observed at burial depths of 130 and 140 m, with 132 and 100 cracks, respectively. For the SVb-type lining, the highest numbers of circumferential cracks were observed at burial depths of 130 and 120 m, with 132 and 66 cracks, respectively.
To compare the probability of longitudinal and circumferential cracks occurring at different burial depths more effectively, statistical analysis was conducted on the quantity of longitudinal and circumferential cracks per kilometer at different burial depths.
As shown in Figure 19, the quantity of longitudinal cracks per kilometer increased with increasing burial depth. For the SIVb-type lining, the longitudinal cracks were slightly affected by the burial depth, whereas for the SVb-type lining, the longitudinal cracks were significantly affected by the burial depth. At burial depths of less than 100 m, the number of longitudinal cracks per kilometer was generally low.

Quantity of longitudinal cracks per kilometer in Wushaoling Tunnel. (a) SIVb-type lining. (b) SVb-type lining.
Figure 20 shows that when the SIVb-type lining was used, the number of circumferential cracks was minimal at a burial depth of 110 m. The number of circumferential cracks increased gradually with the burial depth and reached its peak value at 140 m (approximately 317 cracks per kilometer). For the SVb-type lining, a similar trend was observed. Circumferential cracks were more prevalent at burial depths exceeding 100 m. At a burial depth of 130 m, the maximum number of circumferential cracks was observed (approximately 269 cracks per kilometer).

Number of circumferential cracks per kilometer in Wushaoling Tunnel. (a) SIVb-type lining. (b) SVb-type lining.
5 Tunnel lining crack control technology in high geo-stress environment
5.1 Treatment measures for lining cracks in the Wushaoling tunnel group
Lining damage in tunnels primarily manifests as lining cracking (longitudinal, inclined, and circumferential cracks), lining leakage (minute amount), and thickness defects. To address lining damage and thickness defects, one must first address the cracks and water leakage in the affected areas and then perform structural reinforcement.
5.1.1 Crack disposal methods
For circumferential and longitudinal cracks in the lining, chiseling a “V”-shaped groove along the crack direction for a long crack is recommended. Next holes must be drilled in the groove, grouting pipes inserted into the holes, and epoxy resin-reinforced cement mortar injected for crack plugging. After the epoxy resin mortar achieves a certain strength, cement-water glass slurry or epoxy resin slurry can be injected into the crack, and the treated crack should be observed regularly during tunnel operation.
For other cracks with a width smaller than 0.3 mm, the surface is primarily sealed, and observation should be performed. For cracks with a width exceeding 0.3 mm, low-pressure injection can be employed for reparation.
5.1.2 Tunnel structure reinforcement treatment measurements
Owing to the high geo-stress environment, the tunnel lining of some sections in the Wushaoling tunnel group was severely fractured. Therefore, structural reinforcement is required after the completion of crack treatment to improve the bearing capacity of the lining structure and prevent the continuous development of cracks. Different reinforcement measures were adopted for different lining structure damages. In the Wushaoling tunnel group, four types of reinforcement measures for the tunnel-lining structure were adopted.
Method 1: Implement W-shaped steel-plate reinforcement
The implement W-shaped steel-plate reinforcement method is suitable when minor lining cracks appear. The secondary lining was strengthened by fixing a W-shaped steel plate, which was employed as a circumferential stress strip measuring 20 cm wide, 5 mm thick, and 1.5 m long, with a longitudinal spacing of 60 cm. For the longitudinal connecting steel strip, a W-shaped steel plate measuring 0.8 m long and 0.2 m wide with a ring spacing of 1.3 m was adopted. In addition to the use of a unique steel adhesive to bond the lining concrete firmly, the arch crown and side wall were securely connected to the lining using an adhesive mold expansion anchor bolt with a diameter of 16 mm and an anchorage length of 200 mm. Additionally, two lock foot anchors, each with a length of 3.5 m and a diameter of 28 mm, were added to the arch foot of the tunnel. Finally, polymer mortar was used to smooth the surface of the steel-strip-reinforcement lining.
Method 2: Grouting filling of cavity behind lining
The grouting filling method is suitable when the area and height of the cavity behind the lining are large. For the case where a cavity or an uncompacted area exists behind the lining, holes with a diameter of 50 mm were drilled on the lining within the cavity range and arranged 2 m apart in a rectangular shape. The hole depth was determined by drilling through the lining until the cavity position. When water exists in the cavity behind the hollow lining, the LB-composite (cement based) grouting material should be grouted into the lining using a steel pipe with a diameter of 50 mm. Moreover, piercing the waterproof plate should be avoided when drilling, and waterproof measures should be conducted after grouting.
Grouting was commenced from the side hole at an operating pressure not exceeding 0.1 MPa. When slurry flowed out of the middle hole, it was injected back into the middle hole, and the working pressure was maintained at 0.1 MPa until slurry flowed out of the outlet hole.
Method 3: Using bolt-anchored wire-mesh-based steel-fiber-reinforced shotcrete lining
The section with a slightly smaller lining thickness and intermediate crack damage was strengthened via a treatment method using a bolt-anchored wire-mesh-based steel-fiber-reinforced shotcrete lining, which is shown in Figure 21. For this treatment method, the following rules should be followed.

The treatment method using bolt-anchored wire-mesh-based steel-fiber-reinforced shotcrete lining.
The original secondary lining’s cracks should be repaired, the voids behind the lining backfilled, and the principle of first treating and then reinforcing followed. For local components of the side wall that are extremely thin and thus susceptible to splitting, local replacement should be performed.
The mechanical chiseling anchorage zone concrete lining was brushed or sprayed with a 2 mm interface agent that satisfies type-I index requirements. To enhance the structural integrity and stability of the reinforced lining, a bonded bolt with an expanded bottom was used for anchorage. The anchor bolt was made of stainless steel and featured a nominal diameter of 12 mm. To ensure effective anchorage, the embedment depth was ensured to be at least 100 mm. Additionally, the plum-blossom layout with an anchor distance of 60 cm × 60 cm was adopted to uniformly distribute the anchorage load and minimize stress concentration.
After the anchor bolt installation was completed and had successfully passed the acceptance criteria, a φ12 steel mesh was suspended, with a spacing of 20 cm × 20 cm between each grid. The steel mesh and anchor bolt were cross-bonded with iron wire or spot-welded securely in place. To ensure stability during the lapping process, a U-shaped fixture was set in the lap area to provide a secure fixation.
C30 steel fiber-reinforced concrete (under a standard 28-day curing period with a compressive strength of 30 MPa) was used to achieve a 10 cm-thick spray layer. The volume fraction of steel fiber in the steel fiber-reinforced concrete was 1.0%.
Finally, polymer mortar was used to flatten the surface from the side wall to the hance, and a tunnel fire retardant coating was sprayed on the entire section.
Method 4: Treatment method using lining steel rail and hanging net sprayed concrete lining
For the section with the thin lining thickness, although the cracking damage is serious under the condition of high ground stress, the structure has not lost the bearing capacity, which can be reinforced by steel rail and hanging net sprayed concrete lining. The profile of the lining reinforced by this treatment method is shown in Figure 22.

Treatment method using lining steel rail and hanging net sprayed concrete lining.
The treatment method should meet the following parameter design requirements.
The rail was configured with a longitudinal spacing of 60 cm and was reliably fixed with the existing lining using a φ16U stirrup. The steel rail was made of 55Q15 grade light steel (with a tensile strength of at least 685 MPa), which satisfies the requirements of the code “Hot-rolled light rails GB/T 11264-2012” [41]. The arch foot of the rail was firmly connected to the existing invert by anchorage steel bars. Additionally, it was anchored by a lock foot anchor pipe measuring 3 m in length, 60 mm in diameter, and 5 mm in thickness. Longitudinal connecting bars with a diameter of 22 mm were set between the rails at a circumferential spacing of 1 m. C30 steel fiber-reinforced concrete was sprayed via wet spraying to achieve a spray layer measuring 12 cm thick.
5.2 Lining crack treatment effect
The finite-element method was used to examine the lining crack treatment effect. Owing to the limitations of the article length, only treatment methods 3 and 4 were investigated.
5.2.1 Numerical model
A numerical model was established using the Midas/GTS NX program to analyze the lining crack treatment effect. The Wushaoling tunnel group was modeled as a single-line double-hole tunnel, and the distance between the left and right tunnels was set as 42 m. The interaction between the tunnels was addressed. Considering the complex conditions in the actual project, the section and stratum of the Wushaoling tunnel were simplified in the numerical study.
The buried depth of the tunnel at the calculated section was approximately 130 m. Based on the tunnel excavation’s influence range, the finite element model was designed to measure 120 and 170 m in the horizontal and vertical directions [42], respectively. A self-weight stress field was imposed on the basic model of the Wushaoling tunnel. When tectonic stress was not considered, the boundary conditions of the model were as follows: the vertical boundary constrains the horizontal displacement, the bottom surface constrains the horizontal and vertical displacement, and the upper surface boundary is the free boundary. These geotechnical materials in the numerical model were simulated using quadrilateral and triangular mixed meshes, with 5,264 nodes and 5,231 elements. Additionally, a local refined mesh was adopted in the calculation area of interest. The calculation model of Method 4 is shown in Figure 23.

Schematic diagram of numerical model (Method 4).
In the numerical model, the anchor bolt reinforcement for improving the mechanical properties of the tunnel lining structure was comprehensively considered [43]. Based on the literature, the elastic modulus of a lining subjected to anchor bolt reinforcement increased by 20% [29,44]. Additionally, the thickness of the lining was increased to simulate the spray layer thickness of the steel fiber concrete. The retaining structure of the tunnel was regarded as an elastic material. The nonvolume, linear elastic beam elements, which can provide bending resistance, were used to simulate the behavior of the primary and secondary linings of the tunnel. The primary and secondary linings of the tunnel measured 0.24 and 0.45 m thick, respectively, and were composed of C25 and C30 concrete, respectively [17]. The embedded truss element was set to simulate the anchor bolts in the initial support of the tunnel. A circular section was adopted for the element section, and the axial stiffness of the latter was equivalent to that of the original anchor bolt of a steel pipe with a diameter of 42 mm and a thickness of 3.25 mm. The mechanical parameters of the supporting structure in the model are listed in Table 6. In the numerical model of Method 4, the light rail was simulated using a beam element, and the elastic constitutive model was adopted. The elastic modulus and Poisson’s ratio were 200 GPa and 0.3, respectively. The standard size of the No. 15 light rail was adopted for the rail section. Based on the example of SVb lining, this study examined the reinforcement mechanism of rail-lining reinforcement treatments. The surrounding-rock grade and mechanical parameters are listed in Table 7.
Mechanical parameters of the supporting structure in the model
Materials | Young’s modulus E (GPa) | Poisson’s ratio μ | Unit weight γ (kN/m3) | Diameter (m) |
---|---|---|---|---|
C25 concrete | 28 | 0.2 | 23 | — |
C30 concrete | 30 | 0.2 | 23.5 | — |
Anchor bolt | 78.5 (equivalent modulus) | 0.3 | 78.5 | 0.042 |
Surrounding rock grade and mechanical parameters
Surrounding rock grade | Unit weight γ (kN/m3) | Young’s modulus E (GPa) | Poisson’s ratio μ | c (kPa) | φ (°) |
---|---|---|---|---|---|
V | 24 | 0.8–1 | 0.4 | 160–200 | 21–27 |
To verify the accuracy of the finite element model and the selected parameters, the calculated values of both treatment methods were compared with the measured values obtained from the treated tunnel section. During the operation of the Wushaoling tunnel group from 2013 to 2017, structural damages such as cracking and pavement heave occurred. However, monitoring data were not recorded in this period, affecting the assessment of the structural health of the tunnel. Therefore, during the tunnel reinforcement projects carried out from 2017 to 2018, the tunnel floor heave was monitored using fiber Bragg grating settlement meters. Based on different reinforcement treatment methods, monitoring results from section XK1866 + 280 to XK1866 + 645 of the down-line of Wushaoling Tunnel 1# (Method 3) and section SK1878 + 393 to SK1878 + 720 of the up-line of Wushaoling Tunnel 2# (Method 4) were selected for comparative analysis (Figure 24). As shown in the figure, the bottom heave values of the tunnel resulting from Methods 3 and 4 did not exceed 5 mm, indicating effective deformation control. Additionally, the tunnel floor heaves in treatment Methods 3 and 4 obtained using finite element method (FEM) were compared. Figure 24 indicates that the measured values of the tunnel floor heave are in good agreement with the calculated values. Based on the above analysis, the accuracy of the finite element model in predicting the mechanical behavior of the treated tunnel was validated.

Comparison between measured and calculated values of tunnel floor heave.
5.2.2 Analysis results
5.2.2.1 Displacement analysis
Figure 25 shows the displacement contours yielded by Methods 3 and 4. As shown in Figure 24, the vertical deformation of the secondary lining structure of the tunnel was effectively controlled. After using treatment Methods 3 and 4 to reinforce the lining, the maximum values of the arch-crown settlement and tunnel floor heave by the secondary lining structure decreased as compared with those before the treatment. Among them, the values of the arch-crown settlement and tunnel floor heave in Method 3 were 1.5 and 4.3 mm, respectively. Owing to the overall reinforcement of the secondary lining structure and the sprayed fiber concrete, the vertical deformation of the tunnel was controlled more effectively compared with the case before the reinforcement. For Method 4, the values of the arch-crown settlement and tunnel floor heave were 1.3 and 4.2 mm, respectively. The treatment via steel rail-lining reinforcement effectively restrained the vertical deformation of the secondary lining structure.

Displacement contour for Methods 3 and 4. (a) Vertical displacement contour for Method 3. (b) Horizontal displacement contour for Method 3. (c) Vertical displacement contour for Method 4. (d) Horizontal displacement contour for Method 4.
The horizontal displacement of the secondary lining caused by tunnel excavation primarily occurred at the side wall and hance of the tunnel. After Method 3 was adopted to reinforce the secondary lining structure, the horizontal displacement at the hance of the secondary lining was 4.9 mm, which was approximately 20.7 mm lower than the horizontal displacement before reinforcement. After the secondary lining structure was reinforced via Method 4, the horizontal displacement at the hance was 5.5 mm, i.e., approximately 20.1 mm lower than the horizontal displacement before reinforcement, which effectively limited the lateral deformation of the tunnel under high geo-stress.
5.2.2.2 Stress analysis
Figure 26 shows the stress contours yielded by Methods 3 and 4. When the steel rail lining reinforcement was adopted for the lining structure, the maximum vertical tensile stress of the secondary lining structure appeared at the hance position. The vertical tensile stresses at the hance for Methods 3 and 4 were approximately 1.4 and 1.6 MPa, respectively, and longitudinal tensile cracks generated easily in the tunnel. The stress mode of the original lining structure improved by adopting the steel rail lining to reinforce the upper section of the tunnel, and the tensile stress of the tunnel hance was shared by the steel rail.

Stress contours for Methods 3 and 4. (a) Vertical stress contour for Method 3. (b) Horizontal stress contour for Method 3. (c) Vertical stress contour for Method 4. (d) Horizontal stress contour for Method 4.
The horizontal stress of the tunnel lining structure reduced significantly, and the internal force in the lining was more reasonable. Because of the treatment, the maximum horizontal compressive stress was transferred from the arch crown to the arch foot. The minimum horizontal tensile stress yielded by Method 3 was 0.70 MPa, which appeared at the hance of the tunnel, whereas the maximum horizontal compressive stress was 10.9 MPa, which appeared in a small area at the arch foot. The horizontal stress of the secondary lining was within the strength of the concrete material presented in the specifications after the treatment using bolt-anchored wire-mesh-based steel-fiber-reinforced shotcrete lining. In Method 4, the upper stress of the tunnel-lining structure improved owing to the steel rail-lining reinforcement. The maximum compressive stress of the tunnel crown reduced from 35 to 12.5 MPa at the arch foot, which effectively overcame the low bearing capacity of the tunnel structure.
5.2.2.3 Comparative analysis of treatment methods
To further analyze the treatment and reinforcement effects of Methods 3 and 4, several critical parameters of the secondary lining structure were analyzed. Subsequently, the numerical calculation results of Methods 3 and 4, as well as the conditions before treatment, were compared. The comparison diagram of the treatment method is shown in Figure 27.

Comparison of different treatment measures (S arch crown is the arch crown settlement; S tunnel floor is the tunnel floor heave; S h-hance is the horizontal displacement at hance; σ h-t-max is the maximum horizontal tensile stress; σ h-c-max is the maximum horizontal compressive stress; σ v-t-max is the maximum vertical tensile stress; σ v-c-max is the maximum vertical compressive stress.).
As shown in Figure 27, Methods 3 and 4 significantly affected the treatment of the tunnel-lining structure, which rendered the stress distribution along the tunnel lining more reasonably, thus enabling deformation and stress reductions by 80–90% and 64–95%, respectively. In particular, for the tunnel floor heave control of the secondary lining structure, the tunnel floor heave measured as high as 48.7 mm before treatment, whereas the tunnel floor heave was only 4.2 mm high after treatment using Method 4.
Compared with the conditions before and after treatment, the difference in the treatment effect between Methods 3 and 4 after treatment was slight. At the hance of the tunnel, the maximum horizontal displacement yielded by Method 4 was 5.5 mm, whereas that yielded by Method 3 was only 4.9 mm. Method 3 reduced the maximum horizontal displacement by 10.9% compared with Method 4. The two methods exerted similar limiting effects on the arch crown settlement and tunnel floor heave, with differences of approximately 0.2 and 0.1 mm, respectively. Compared with Method 3, Method 4 significantly reduced the lining stress. The maximum vertical compressive stress yielded by Method 4 was only 1.3 MPa, which was 43% lower than 2.3 MPa yielded by Method 3.
6 Conclusion
Based on a statistical analysis of the observations obtained from the Wushaoling tunnel group, the distribution characteristics and primary factors of tunnel lining cracks under high geo-stress conditions were investigated. The treatment measures of lining cracks for soft rock tunnels under high geo-stress conditions were proposed. The mechanical performance of different treatment methods was evaluated using FEM. The following conclusions can be drawn:
Under high geo-stress conditions, tunnel lining cracks were mainly circumferential and longitudinal cracks. Circumferential and longitudinal cracks account for approximately 53.2 and 29.4% of the total number of cracks, respectively, and about 54.1 and 30.9% of the total crack length. The areas with a higher occurrence of longitudinal cracks in the tunnel lining also have a higher concentration of circumferential cracks. The longitudinal cracks in the tunnel lining primarily occur near the tunnel crown and hance.
The tunnel lining structure has a significant impact on crack generation, and the closure design of the initial support invert can effectively control the development of tunnel cracks. The SIVb-, SVc-, and SVd-type linings showed a high number of longitudinal cracks per kilometer. In terms of the lining types in Grade V surrounding rocks, the number of longitudinal cracks per kilometer increased with an increase in the lining grade. When tunnel burial depths exceed 100 m, the number of longitudinal and circumferential cracks per kilometer increased gradually with the burial depth of the tunnel.
Based on the structural damage characteristics of the Wushaoling tunnel lining, four tunnel structure reinforcement treatment measurements for lining cracks in high geo-stress condition were innovatively proposed, including Implement W-shaped steel-plate reinforcement, grouting filling of cavity behind lining, using bolt-anchored wire-mesh-based steel-fiber-reinforced shotcrete lining, and treatment method using lining steel rail and hanging net sprayed concrete lining.
The mechanical performance of the tunnel reinforcement treatment measurements was investigated using FEM. The calculated results indicate that both treatment measurements, using bolt-anchored wire-mesh-based steel-fiber-reinforced shotcrete lining (Method 3) and treatment method using lining steel rail and hanging net sprayed concrete lining (Method 4), resulted in a more reliable stress distribution of the tunnel linings. The location of the maximum horizontal pressure stress shifted from the tunnel crown to the arch foot after treatment, resulting in an 80–90% reduction in deformation and a 64–95% reduction in stress compared with the case before treatment. In terms of controlling the heave of the tunnel invert in the secondary lining structure, the two treatment measurements reduced the tunnel heave by 44.5 mm.
While for the generation mechanism of different types of tunnel crack, such as the tensile crack and shear crack, further analyses are needed to obtain the crack evolution and control technologies in engineering practice. The effective crack control technologies for tunnel lining in high geo-stress conditions are still of particular concern and deserves further study.
Acknowledgements
This work was supported by the Key Research and Development Program of Gansu Province, China (Grants 22YF7FH224), the Xi’an Association for Science and Technology Young Talent Support Program Project (095920221358), Shaanxi Province Postdoctoral Research Project Funding (2023BSHYDZZ138), Shandong Youth Innovation Team (No. 2023KJ324), Open Program of Engineering Research Center of Concrete Technology under Marine Environment, Ministry of Education (Grants 2024KFKT-YB12) and the Doctoral Research Fund of Shandong Jianzhu University (Grant no X19080Z). We deeply appreciate the warm and efficient work by editors and reviewers.
-
Author contributions: All authors have accepted responsibility for the entire content of this manuscript and consented to its submission to the journal, reviewed all the results and approved the final version of the manuscript. J.H.: conceptualization, methodology, software, funding acquisition, writing – original draft, and writing – review and editing. D.L.: data curation, formal analysis, writing – original draft, investigation, software, and writing – review and editing. S.Z.: supervision, investigation, project administration, resource, and writing – review and editing. Y.C.: supervision, validation, formal analysis, funding acquisition, investigation, writing – original draft, and writing – review and editing. Y.Z.: data curation, investigation, resources, visualization, and writing – review and editing. L.Z.: data curation, investigation, and language editing. C.H.: data curation, formal analysis, and writing – review and editing. M.Z.: investigation, validation, and writing – review and editing.
-
Conflict of interest: Authors state no conflict of interest.
-
Data availability statement: The datasets generated during and/or analyzed during the current study are available from the corresponding author on reasonable request.
References
[1] Editorial Department of China Journal of Highway and Transport. Review on China’s tunnel engineering research: 2015. China J Highw Transp. 2015;28(5):1–65 (in Chinese).Search in Google Scholar
[2] He M, Jing H, Sun X. Engineering mechanics of soft rock. Beijing: Science Press; 2002 (in Chinese).Search in Google Scholar
[3] Zhou Y, Yang W, Zhao L, Zhang Y, Tian H, Zhang L, et al. Research on reasonable reserved deformation and height-span ratio of a large deformation tunnel section in high geo-stress soft rock near a fault zone: A case study. Bull Eng Geol Environ. 2023;82(10):378.10.1007/s10064-023-03407-wSearch in Google Scholar
[4] Ma D, Tan Z, Bian L, Zhang B, Zhao J. Research on deformation and loose zone characteristics of large cross section tunnel in high geo-stress soft rock. Appl Sci. 2023;13(15):9009.10.3390/app13159009Search in Google Scholar
[5] Liu W, Chen J, Luo Y, Chen L, Zhang L, He C, et al. Long-term stress monitoring and in-service durability evaluation of a large-span tunnel in squeezing rock. Tunn Undergr Space Technol. 2022;127:104611.10.1016/j.tust.2022.104611Search in Google Scholar
[6] Zhou Z, Chen Z, He C, Kou H. Investigation on the evolution characteristics and transfer mechanism of surrounding rock pressure for a hard-rock tunnel under high geo-stress: case study on the Erlang Mountain Tunnel, China. Bull Eng Geol Environ. 2021;80(11):8339–61.10.1007/s10064-021-02439-4Search in Google Scholar
[7] Chen Y, Zhang R, Zi J, Han J, Liu K. Evaluation of the treatment variables on the shear strength of MICP-treated loess. J Mt Sci. 2024;21. 10.1007/s11629-024-9100-3.Search in Google Scholar
[8] Duan S, Gao P, Xu D, Cao B, Liu G, Jiang Q, et al. A new perspective on the semi-quantitative meso-structural failure mechanism of deep weak interlayer zone under different stress paths. Rock Mech Rock Eng. 2024;57:3171–95.10.1007/s00603-024-03760-6Search in Google Scholar
[9] Zhao J, Jiang Q, Lu J, Chen B, Pei S, Wang Z. Rock fracturing observation based on microseismic monitoring and borehole imaging: In situ investigation in a large underground cavern under high geostress. Tunn Undergr Space Technol. 2022;126:104549.10.1016/j.tust.2022.104549Search in Google Scholar
[10] Zhao J, Chen B, Jiang Q, Xu D, He B, Duan S. In-situ comprehensive investigation of deformation mechanism of the rock mass with weak interlayer zone in the Baihetan Hydropower Station. Tunn Undergr Space Technol. 2024;148:105690.10.1016/j.tust.2024.105690Search in Google Scholar
[11] Zhao J, Tan Z, Zhang B, Wang F. Stress-release technology and engineering application of advanced center drifts in a super-deep soft-rock tunnel: A case study of the Haba Snow Mountain Tunnel. Rock Mech Rock Eng. 2024;57(9):7103–24.10.1007/s00603-024-03899-2Search in Google Scholar
[12] Zhang B, Tan Z, Zhao J, Wang F, Lin K. Research on stress field inversion and large deformation level determination of super deep buried soft rock tunnel. Sci Rep. 2024;14(1):12739.10.1038/s41598-024-62597-9Search in Google Scholar PubMed PubMed Central
[13] Jiang Q, Zhong S, Pan P, Shi Y, Guo H, Kou Y. Observe the temporal evolution of deep tunnel’s 3D deformation by 3D laser scanning in the Jinchuan No. 2 Mine. Tunn Undergr Space Technol. 2020;97:103237.10.1016/j.tust.2019.103237Search in Google Scholar
[14] John M. Construction of the Arlberg Expressway Tunnel Tube-4. Tunn Tunn Int. 1980;6(12):66–8.Search in Google Scholar
[15] Ayaydin N. First and second tube of the Tauern Tunnel. Geomechanik Tunnelbau. 2010;4:334–43.10.1002/geot.201090029Search in Google Scholar
[16] Yu W, Wang B, Zi X, Guo X, Wang Z. Effect of prestressed anchorage system on mechanical behavior of squeezed softrock in large-deformation tunnel. Tunn Undergr Space Technol. 2023;131:104782.10.1016/j.tust.2022.104782Search in Google Scholar
[17] Li J, Wang Z, Wang Y. Analysis and countermeasures of large deformation of deep-buried tunnel excavated in layered rock strata: A case study. Eng Fail Anal. 2023;146:107057.10.1016/j.engfailanal.2023.107057Search in Google Scholar
[18] Dai G, Zhu H, Xia C. Study on causation of highway tunnel defects and their countermeasures. China Saf Sci J. 2005;12:89–92 (in Chinese).Search in Google Scholar
[19] Xue G, Gu C, Fang X, Wei T. A case study on large deformation failure mechanism and control techniques for soft rock roadways in tectonic stress areas. Sustainability. 2019;11(13):3510.10.3390/su11133510Search in Google Scholar
[20] Wang J. Study on the mechanism and treatment measures of large deformation of soft rock deformation of tunnel of Xuecheng national road G317. Chengdu, China: Chengdu University of Technology; 2017 (in Chinese).Search in Google Scholar
[21] Zhao J, Tan Z, Li L, Wang X. Supporting structure failure caused by the squeezing tunnel creep and its reinforcement measure. J Mt Sci. 2023;20(6):1774–89.10.1007/s11629-022-7853-0Search in Google Scholar
[22] Chuang S, Dongxu C, Laigui W, Lin W. Quantitative evaluation of the constraint effect and stability of tunnel lining support. Tunn Undergr Space Technol. 2021;112:103920.10.1016/j.tust.2021.103920Search in Google Scholar
[23] Bian K, Liu J, Liu Z, Liu S, Ai F, Zheng X, et al. Mechanisms of large deformation in soft rock tunnels: a case study of Huangjiazhai Tunnel. Bull Eng Geol Environ. 2019;78(1):431–44.10.1007/s10064-017-1155-8Search in Google Scholar
[24] Zhao J, Tan Z, Wang W, Yu R, Wang J, Li Z. Study on the large deformation control technology of a single-hole double-track railway tunnel. Bull Eng Geol Environ. 2023;82(9):343.10.1007/s10064-023-03375-1Search in Google Scholar
[25] Liu Z. Study on the mechanical behavior of double primary support of soft rock tunnel under high ground stresses and large deformation. Adv Civ Eng. 2020;8832797.10.1155/2020/8832797Search in Google Scholar
[26] Chen Z, He C, Xu G, Ma G, Yang W. Supporting mechanism and mechanical behavior of a double primary support method for tunnels in broken phyllite under high geo-stress: a case study. Bull Eng Geol Environ. 2019;78(7):5253–67.10.1007/s10064-019-01479-1Search in Google Scholar
[27] Li L, Tan Z, Guo X, Wu Y, Luo N. Large deformation of tunnels in steep dip strata of interbedding phyllite under high geo-stresses. Chin J Rock Mech Eng. 2017;36(7):1611–22 (in Chinese).Search in Google Scholar
[28] Xu P, Wei Y, Yang Y, Zhou X. Application of fabricated corrugated steel plate in subway tunnel supporting structure. Case Stud Constr Mater. 2022;17:e1323.10.1016/j.cscm.2022.e01323Search in Google Scholar
[29] Miao C, Jiang M, Li Z, Sun X, Zhang T, Zhang Y, et al. Numerical simulation of rockburst disaster and control strategy of constant resistance and large deformation anchor cable in Gaoloushan tunnel. J Mt Sci. 2023;20(6):1605–19.10.1007/s11629-023-7916-xSearch in Google Scholar
[30] Tao Z, Cao J, Yang L, Guo A, Huang R, Yang X, et al. Study on deformation mechanism and support measures of soft surrounding rock in Muzhailing deep tunnel. Adv Civ Eng. 2020;2020:1–14.10.1155/2020/9367916Search in Google Scholar
[31] He C, Tang Z, Wang B, Wang Y, She J. Research on effect of inner surface reinforcing on structure bearing capacity by model test in defective tunnel. Rock Soil Mech. 2009;30(2):406–12 (in Chinese).Search in Google Scholar
[32] Zhang C, Tan X, Tian H, Chen W. Lateral compression and energy absorption of foamed concrete-filled polyethylene circular pipe as yielding layer for high geo-stress soft rock tunnels. Int J Min Sci Technol. 2022;32(5):1087–96.10.1016/j.ijmst.2022.08.011Search in Google Scholar
[33] Wei L, Zhou X. Analysis and countermeasures for inverted arch diseases in high geostress section of railway tunnel in plateau and cold region: A case study on Muzhailing tunnel of Lanzhou-Chongqing railway. Tunn Constr. 2020;40(S2):249–55 (in Chinese).Search in Google Scholar
[34] Chongqing Jiaotong Research & Design Institute Co., Ltd. Code for design of road tunnel JTG D70-2004. Beijing: People’s Comunications Press; 2004 (in Chinese).Search in Google Scholar
[35] Ministry of Housing and Urban-Rural Development of the People’s Republic of China (MOHURD). Standard for engineering classification of rock mass GB/T 50218-2014. Beijing: China Planning Press; 2014 (in Chinese).Search in Google Scholar
[36] Ministry of Transport of the People’s Republic of China. Specifications for Design of Highway Tunnels JTG D70-2014. Beijing: China Communications Press; 2014.Search in Google Scholar
[37] Huang C, Li S, Li G, Yao T, Wu X. Reform of deformation control technology for railway tunnels with squeezing surrounding rock: case study of the new and existing Wushaoling tunnels in China. Front Earth Sci. 2005;12:1438425.10.3389/feart.2024.1438425Search in Google Scholar
[38] Zhang S, Zhu Y, Liu Z. Large extrusion deflection control technology for tunnel in active fault zone. Appl Mech Mater. 2011;90:1824–7.10.4028/www.scientific.net/AMM.90-93.1824Search in Google Scholar
[39] Zhao X, Chen H, Wang C. Resistance of large deformation of the Wushaoling Tunnel F7 soft fault. Front Archit Civ Eng China. 2007;1:123–7.10.1007/s11709-007-0013-3Search in Google Scholar
[40] Liu Z, Li W, Zhang S, Zhu Y. Synthetical analysis on monitoring of Wushaoling railway tunnel. Tunn Undergr Space Technol Incorporating Trenchless Technol Res. 2006;21(3):363–4.10.1016/j.tust.2005.12.180Search in Google Scholar
[41] General Administration of Quality Supervision, Inspection and Quarantine of the People’s Republic of China. Hot-rolled light rails. Beijing: China Standards Press; 2012.Search in Google Scholar
[42] Han J, Wang J, Cheng C, Zhang C, Liang E, Wang Z, et al. Mechanical response and parametric analysis of a deep excavation structure overlying an existing subway station: A case study of the Beijing subway station expansion. Front Earth Sci. 2023;10:1079837.10.3389/feart.2022.1079837Search in Google Scholar
[43] Han J, Wang J, Jia D, Yan F, Zhao Y, Bai X, et al. Construction technologies and mechanical effects of the pipe-jacking crossing anchor-cable group in soft stratum. Front Earth Sci. 2023;10:1019801.10.3389/feart.2022.1019801Search in Google Scholar
[44] Feng J, Tan Y, Yao S, Jiang H, Zhang J, Li H. Study on stress variation of advance fiberglass anchor bolts during tunnel excavation process. Sci Rep. 2023;13(1):4173.10.1038/s41598-023-31000-4Search in Google Scholar PubMed PubMed Central
© 2024 the author(s), published by De Gruyter
This work is licensed under the Creative Commons Attribution 4.0 International License.
Articles in the same Issue
- Regular Articles
- Theoretical magnetotelluric response of stratiform earth consisting of alternative homogeneous and transitional layers
- The research of common drought indexes for the application to the drought monitoring in the region of Jin Sha river
- Evolutionary game analysis of government, businesses, and consumers in high-standard farmland low-carbon construction
- On the use of low-frequency passive seismic as a direct hydrocarbon indicator: A case study at Banyubang oil field, Indonesia
- Water transportation planning in connection with extreme weather conditions; case study – Port of Novi Sad, Serbia
- Zircon U–Pb ages of the Paleozoic volcaniclastic strata in the Junggar Basin, NW China
- Monitoring of mangrove forests vegetation based on optical versus microwave data: A case study western coast of Saudi Arabia
- Microfacies analysis of marine shale: A case study of the shales of the Wufeng–Longmaxi formation in the western Chongqing, Sichuan Basin, China
- Multisource remote sensing image fusion processing in plateau seismic region feature information extraction and application analysis – An example of the Menyuan Ms6.9 earthquake on January 8, 2022
- Identification of magnetic mineralogy and paleo-flow direction of the Miocene-quaternary volcanic products in the north of Lake Van, Eastern Turkey
- Impact of fully rotating steel casing bored pile on adjacent tunnels
- Adolescents’ consumption intentions toward leisure tourism in high-risk leisure environments in riverine areas
- Petrogenesis of Jurassic granitic rocks in South China Block: Implications for events related to subduction of Paleo-Pacific plate
- Differences in urban daytime and night block vitality based on mobile phone signaling data: A case study of Kunming’s urban district
- Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan
- Integrated geophysical approach for detection and size-geometry characterization of a multiscale karst system in carbonate units, semiarid Brazil
- Spatial and temporal changes in ecosystem services value and analysis of driving factors in the Yangtze River Delta Region
- Deep fault sliding rates for Ka-Ping block of Xinjiang based on repeating earthquakes
- Improved deep learning segmentation of outdoor point clouds with different sampling strategies and using intensities
- Platform margin belt structure and sedimentation characteristics of Changxing Formation reefs on both sides of the Kaijiang-Liangping trough, eastern Sichuan Basin, China
- Enhancing attapulgite and cement-modified loess for effective landfill lining: A study on seepage prevention and Cu/Pb ion adsorption
- Flood risk assessment, a case study in an arid environment of Southeast Morocco
- Lower limits of physical properties and classification evaluation criteria of the tight reservoir in the Ahe Formation in the Dibei Area of the Kuqa depression
- Evaluation of Viaducts’ contribution to road network accessibility in the Yunnan–Guizhou area based on the node deletion method
- Permian tectonic switch of the southern Central Asian Orogenic Belt: Constraints from magmatism in the southern Alxa region, NW China
- Element geochemical differences in lower Cambrian black shales with hydrothermal sedimentation in the Yangtze block, South China
- Three-dimensional finite-memory quasi-Newton inversion of the magnetotelluric based on unstructured grids
- Obliquity-paced summer monsoon from the Shilou red clay section on the eastern Chinese Loess Plateau
- Classification and logging identification of reservoir space near the upper Ordovician pinch-out line in Tahe Oilfield
- Ultra-deep channel sand body target recognition method based on improved deep learning under UAV cluster
- New formula to determine flyrock distance on sedimentary rocks with low strength
- Assessing the ecological security of tourism in Northeast China
- Effective reservoir identification and sweet spot prediction in Chang 8 Member tight oil reservoirs in Huanjiang area, Ordos Basin
- Detecting heterogeneity of spatial accessibility to sports facilities for adolescents at fine scale: A case study in Changsha, China
- Effects of freeze–thaw cycles on soil nutrients by soft rock and sand remodeling
- Vibration prediction with a method based on the absorption property of blast-induced seismic waves: A case study
- A new look at the geodynamic development of the Ediacaran–early Cambrian forearc basalts of the Tannuola-Khamsara Island Arc (Central Asia, Russia): Conclusions from geological, geochemical, and Nd-isotope data
- Spatio-temporal analysis of the driving factors of urban land use expansion in China: A study of the Yangtze River Delta region
- Selection of Euler deconvolution solutions using the enhanced horizontal gradient and stable vertical differentiation
- Phase change of the Ordovician hydrocarbon in the Tarim Basin: A case study from the Halahatang–Shunbei area
- Using interpretative structure model and analytical network process for optimum site selection of airport locations in Delta Egypt
- Geochemistry of magnetite from Fe-skarn deposits along the central Loei Fold Belt, Thailand
- Functional typology of settlements in the Srem region, Serbia
- Hunger Games Search for the elucidation of gravity anomalies with application to geothermal energy investigations and volcanic activity studies
- Addressing incomplete tile phenomena in image tiling: Introducing the grid six-intersection model
- Evaluation and control model for resilience of water resource building system based on fuzzy comprehensive evaluation method and its application
- MIF and AHP methods for delineation of groundwater potential zones using remote sensing and GIS techniques in Tirunelveli, Tenkasi District, India
- New database for the estimation of dynamic coefficient of friction of snow
- Measuring urban growth dynamics: A study in Hue city, Vietnam
- Comparative models of support-vector machine, multilayer perceptron, and decision tree predication approaches for landslide susceptibility analysis
- Experimental study on the influence of clay content on the shear strength of silty soil and mechanism analysis
- Geosite assessment as a contribution to the sustainable development of Babušnica, Serbia
- Using fuzzy analytical hierarchy process for road transportation services management based on remote sensing and GIS technology
- Accumulation mechanism of multi-type unconventional oil and gas reservoirs in Northern China: Taking Hari Sag of the Yin’e Basin as an example
- TOC prediction of source rocks based on the convolutional neural network and logging curves – A case study of Pinghu Formation in Xihu Sag
- A method for fast detection of wind farms from remote sensing images using deep learning and geospatial analysis
- Spatial distribution and driving factors of karst rocky desertification in Southwest China based on GIS and geodetector
- Physicochemical and mineralogical composition studies of clays from Share and Tshonga areas, Northern Bida Basin, Nigeria: Implications for Geophagia
- Geochemical sedimentary records of eutrophication and environmental change in Chaohu Lake, East China
- Research progress of freeze–thaw rock using bibliometric analysis
- Mixed irrigation affects the composition and diversity of the soil bacterial community
- Examining the swelling potential of cohesive soils with high plasticity according to their index properties using GIS
- Geological genesis and identification of high-porosity and low-permeability sandstones in the Cretaceous Bashkirchik Formation, northern Tarim Basin
- Usability of PPGIS tools exemplified by geodiscussion – a tool for public participation in shaping public space
- Efficient development technology of Upper Paleozoic Lower Shihezi tight sandstone gas reservoir in northeastern Ordos Basin
- Assessment of soil resources of agricultural landscapes in Turkestan region of the Republic of Kazakhstan based on agrochemical indexes
- Evaluating the impact of DEM interpolation algorithms on relief index for soil resource management
- Petrogenetic relationship between plutonic and subvolcanic rocks in the Jurassic Shuikoushan complex, South China
- A novel workflow for shale lithology identification – A case study in the Gulong Depression, Songliao Basin, China
- Characteristics and main controlling factors of dolomite reservoirs in Fei-3 Member of Feixianguan Formation of Lower Triassic, Puguang area
- Impact of high-speed railway network on county-level accessibility and economic linkage in Jiangxi Province, China: A spatio-temporal data analysis
- Estimation model of wild fractional vegetation cover based on RGB vegetation index and its application
- Lithofacies, petrography, and geochemistry of the Lamphun oceanic plate stratigraphy: As a record of the subduction history of Paleo-Tethys in Chiang Mai-Chiang Rai Suture Zone of Thailand
- Structural features and tectonic activity of the Weihe Fault, central China
- Application of the wavelet transform and Hilbert–Huang transform in stratigraphic sequence division of Jurassic Shaximiao Formation in Southwest Sichuan Basin
- Structural detachment influences the shale gas preservation in the Wufeng-Longmaxi Formation, Northern Guizhou Province
- Distribution law of Chang 7 Member tight oil in the western Ordos Basin based on geological, logging and numerical simulation techniques
- Evaluation of alteration in the geothermal province west of Cappadocia, Türkiye: Mineralogical, petrographical, geochemical, and remote sensing data
- Numerical modeling of site response at large strains with simplified nonlinear models: Application to Lotung seismic array
- Quantitative characterization of granite failure intensity under dynamic disturbance from energy standpoint
- Characteristics of debris flow dynamics and prediction of the hazardous area in Bangou Village, Yanqing District, Beijing, China
- Rockfall mapping and susceptibility evaluation based on UAV high-resolution imagery and support vector machine method
- Statistical comparison analysis of different real-time kinematic methods for the development of photogrammetric products: CORS-RTK, CORS-RTK + PPK, RTK-DRTK2, and RTK + DRTK2 + GCP
- Hydrogeological mapping of fracture networks using earth observation data to improve rainfall–runoff modeling in arid mountains, Saudi Arabia
- Petrography and geochemistry of pegmatite and leucogranite of Ntega-Marangara area, Burundi, in relation to rare metal mineralisation
- Prediction of formation fracture pressure based on reinforcement learning and XGBoost
- Hazard zonation for potential earthquake-induced landslide in the eastern East Kunlun fault zone
- Monitoring water infiltration in multiple layers of sandstone coal mining model with cracks using ERT
- Study of the patterns of ice lake variation and the factors influencing these changes in the western Nyingchi area
- Productive conservation at the landslide prone area under the threat of rapid land cover changes
- Sedimentary processes and patterns in deposits corresponding to freshwater lake-facies of hyperpycnal flow – An experimental study based on flume depositional simulations
- Study on time-dependent injectability evaluation of mudstone considering the self-healing effect
- Detection of objects with diverse geometric shapes in GPR images using deep-learning methods
- Behavior of trace metals in sedimentary cores from marine and lacustrine environments in Algeria
- Spatiotemporal variation pattern and spatial coupling relationship between NDVI and LST in Mu Us Sandy Land
- Formation mechanism and oil-bearing properties of gravity flow sand body of Chang 63 sub-member of Yanchang Formation in Huaqing area, Ordos Basin
- Diagenesis of marine-continental transitional shale from the Upper Permian Longtan Formation in southern Sichuan Basin, China
- Vertical high-velocity structures and seismic activity in western Shandong Rise, China: Case study inspired by double-difference seismic tomography
- Spatial coupling relationship between metamorphic core complex and gold deposits: Constraints from geophysical electromagnetics
- Disparities in the geospatial allocation of public facilities from the perspective of living circles
- Research on spatial correlation structure of war heritage based on field theory. A case study of Jinzhai County, China
- Formation mechanisms of Qiaoba-Zhongdu Danxia landforms in southwestern Sichuan Province, China
- Magnetic data interpretation: Implication for structure and hydrocarbon potentiality at Delta Wadi Diit, Southeastern Egypt
- Deeply buried clastic rock diagenesis evolution mechanism of Dongdaohaizi sag in the center of Junggar fault basin, Northwest China
- Application of LS-RAPID to simulate the motion of two contrasting landslides triggered by earthquakes
- The new insight of tectonic setting in Sunda–Banda transition zone using tomography seismic. Case study: 7.1 M deep earthquake 29 August 2023
- The critical role of c and φ in ensuring stability: A study on rockfill dams
- Evidence of late quaternary activity of the Weining-Shuicheng Fault in Guizhou, China
- Extreme hydroclimatic events and response of vegetation in the eastern QTP since 10 ka
- Spatial–temporal effect of sea–land gradient on landscape pattern and ecological risk in the coastal zone: A case study of Dalian City
- Study on the influence mechanism of land use on carbon storage under multiple scenarios: A case study of Wenzhou
- A new method for identifying reservoir fluid properties based on well logging data: A case study from PL block of Bohai Bay Basin, North China
- Comparison between thermal models across the Middle Magdalena Valley, Eastern Cordillera, and Eastern Llanos basins in Colombia
- Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts
- Chlorite-induced porosity evolution in multi-source tight sandstone reservoirs: A case study of the Shaximiao Formation in western Sichuan Basin
- Predicting stability factors for rotational failures in earth slopes and embankments using artificial intelligence techniques
- Origin of Late Cretaceous A-type granitoids in South China: Response to the rollback and retreat of the Paleo-Pacific plate
- Modification of dolomitization on reservoir spaces in reef–shoal complex: A case study of Permian Changxing Formation, Sichuan Basin, SW China
- Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration
- Rock physics model for deep coal-bed methane reservoir based on equivalent medium theory: A case study of Carboniferous-Permian in Eastern Ordos Basin
- Enhancing the total-field magnetic anomaly using the normalized source strength
- Shear wave velocity profiling of Riyadh City, Saudi Arabia, utilizing the multi-channel analysis of surface waves method
- Effect of coal facies on pore structure heterogeneity of coal measures: Quantitative characterization and comparative study
- Inversion method of organic matter content of different types of soils in black soil area based on hyperspectral indices
- Detection of seepage zones in artificial levees: A case study at the Körös River, Hungary
- Tight sandstone fluid detection technology based on multi-wave seismic data
- Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
- Influence of pore structure characteristics on the Permian Shan-1 reservoir in Longdong, Southwest Ordos Basin, China
- Study on sedimentary model of Shanxi Formation – Lower Shihezi Formation in Da 17 well area of Daniudi gas field, Ordos Basin
- Multi-scenario territorial spatial simulation and dynamic changes: A case study of Jilin Province in China from 1985 to 2030
- Review Articles
- Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
- Prediction and assessment of meteorological drought in southwest China using long short-term memory model
- Communication
- Essential questions in earth and geosciences according to large language models
- Erratum
- Erratum to “Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan”
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part I
- Spatial-temporal and trend analysis of traffic accidents in AP Vojvodina (North Serbia)
- Exploring environmental awareness, knowledge, and safety: A comparative study among students in Montenegro and North Macedonia
- Determinants influencing tourists’ willingness to visit Türkiye – Impact of earthquake hazards on Serbian visitors’ preferences
- Application of remote sensing in monitoring land degradation: A case study of Stanari municipality (Bosnia and Herzegovina)
- Optimizing agricultural land use: A GIS-based assessment of suitability in the Sana River Basin, Bosnia and Herzegovina
- Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index
- Analysis of the intensity of erosive processes and state of vegetation cover in the zone of influence of the Kolubara Mining Basin
- GIS-based spatial modeling of landslide susceptibility using BWM-LSI: A case study – city of Smederevo (Serbia)
- Geospatial modeling of wildfire susceptibility on a national scale in Montenegro: A comparative evaluation of F-AHP and FR methodologies
- Geosite assessment as the first step for the development of canyoning activities in North Montenegro
- Urban geoheritage and degradation risk assessment of the Sokograd fortress (Sokobanja, Eastern Serbia)
- Multi-hazard modeling of erosion and landslide susceptibility at the national scale in the example of North Macedonia
- Understanding seismic hazard resilience in Montenegro: A qualitative analysis of community preparedness and response capabilities
- Forest soil CO2 emission in Quercus robur level II monitoring site
- Characterization of glomalin proteins in soil: A potential indicator of erosion intensity
- Power of Terroir: Case study of Grašac at the Fruška Gora wine region (North Serbia)
- Special Issue: Geospatial and Environmental Dynamics - Part I
- Qualitative insights into cultural heritage protection in Serbia: Addressing legal and institutional gaps for disaster risk resilience
Articles in the same Issue
- Regular Articles
- Theoretical magnetotelluric response of stratiform earth consisting of alternative homogeneous and transitional layers
- The research of common drought indexes for the application to the drought monitoring in the region of Jin Sha river
- Evolutionary game analysis of government, businesses, and consumers in high-standard farmland low-carbon construction
- On the use of low-frequency passive seismic as a direct hydrocarbon indicator: A case study at Banyubang oil field, Indonesia
- Water transportation planning in connection with extreme weather conditions; case study – Port of Novi Sad, Serbia
- Zircon U–Pb ages of the Paleozoic volcaniclastic strata in the Junggar Basin, NW China
- Monitoring of mangrove forests vegetation based on optical versus microwave data: A case study western coast of Saudi Arabia
- Microfacies analysis of marine shale: A case study of the shales of the Wufeng–Longmaxi formation in the western Chongqing, Sichuan Basin, China
- Multisource remote sensing image fusion processing in plateau seismic region feature information extraction and application analysis – An example of the Menyuan Ms6.9 earthquake on January 8, 2022
- Identification of magnetic mineralogy and paleo-flow direction of the Miocene-quaternary volcanic products in the north of Lake Van, Eastern Turkey
- Impact of fully rotating steel casing bored pile on adjacent tunnels
- Adolescents’ consumption intentions toward leisure tourism in high-risk leisure environments in riverine areas
- Petrogenesis of Jurassic granitic rocks in South China Block: Implications for events related to subduction of Paleo-Pacific plate
- Differences in urban daytime and night block vitality based on mobile phone signaling data: A case study of Kunming’s urban district
- Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan
- Integrated geophysical approach for detection and size-geometry characterization of a multiscale karst system in carbonate units, semiarid Brazil
- Spatial and temporal changes in ecosystem services value and analysis of driving factors in the Yangtze River Delta Region
- Deep fault sliding rates for Ka-Ping block of Xinjiang based on repeating earthquakes
- Improved deep learning segmentation of outdoor point clouds with different sampling strategies and using intensities
- Platform margin belt structure and sedimentation characteristics of Changxing Formation reefs on both sides of the Kaijiang-Liangping trough, eastern Sichuan Basin, China
- Enhancing attapulgite and cement-modified loess for effective landfill lining: A study on seepage prevention and Cu/Pb ion adsorption
- Flood risk assessment, a case study in an arid environment of Southeast Morocco
- Lower limits of physical properties and classification evaluation criteria of the tight reservoir in the Ahe Formation in the Dibei Area of the Kuqa depression
- Evaluation of Viaducts’ contribution to road network accessibility in the Yunnan–Guizhou area based on the node deletion method
- Permian tectonic switch of the southern Central Asian Orogenic Belt: Constraints from magmatism in the southern Alxa region, NW China
- Element geochemical differences in lower Cambrian black shales with hydrothermal sedimentation in the Yangtze block, South China
- Three-dimensional finite-memory quasi-Newton inversion of the magnetotelluric based on unstructured grids
- Obliquity-paced summer monsoon from the Shilou red clay section on the eastern Chinese Loess Plateau
- Classification and logging identification of reservoir space near the upper Ordovician pinch-out line in Tahe Oilfield
- Ultra-deep channel sand body target recognition method based on improved deep learning under UAV cluster
- New formula to determine flyrock distance on sedimentary rocks with low strength
- Assessing the ecological security of tourism in Northeast China
- Effective reservoir identification and sweet spot prediction in Chang 8 Member tight oil reservoirs in Huanjiang area, Ordos Basin
- Detecting heterogeneity of spatial accessibility to sports facilities for adolescents at fine scale: A case study in Changsha, China
- Effects of freeze–thaw cycles on soil nutrients by soft rock and sand remodeling
- Vibration prediction with a method based on the absorption property of blast-induced seismic waves: A case study
- A new look at the geodynamic development of the Ediacaran–early Cambrian forearc basalts of the Tannuola-Khamsara Island Arc (Central Asia, Russia): Conclusions from geological, geochemical, and Nd-isotope data
- Spatio-temporal analysis of the driving factors of urban land use expansion in China: A study of the Yangtze River Delta region
- Selection of Euler deconvolution solutions using the enhanced horizontal gradient and stable vertical differentiation
- Phase change of the Ordovician hydrocarbon in the Tarim Basin: A case study from the Halahatang–Shunbei area
- Using interpretative structure model and analytical network process for optimum site selection of airport locations in Delta Egypt
- Geochemistry of magnetite from Fe-skarn deposits along the central Loei Fold Belt, Thailand
- Functional typology of settlements in the Srem region, Serbia
- Hunger Games Search for the elucidation of gravity anomalies with application to geothermal energy investigations and volcanic activity studies
- Addressing incomplete tile phenomena in image tiling: Introducing the grid six-intersection model
- Evaluation and control model for resilience of water resource building system based on fuzzy comprehensive evaluation method and its application
- MIF and AHP methods for delineation of groundwater potential zones using remote sensing and GIS techniques in Tirunelveli, Tenkasi District, India
- New database for the estimation of dynamic coefficient of friction of snow
- Measuring urban growth dynamics: A study in Hue city, Vietnam
- Comparative models of support-vector machine, multilayer perceptron, and decision tree predication approaches for landslide susceptibility analysis
- Experimental study on the influence of clay content on the shear strength of silty soil and mechanism analysis
- Geosite assessment as a contribution to the sustainable development of Babušnica, Serbia
- Using fuzzy analytical hierarchy process for road transportation services management based on remote sensing and GIS technology
- Accumulation mechanism of multi-type unconventional oil and gas reservoirs in Northern China: Taking Hari Sag of the Yin’e Basin as an example
- TOC prediction of source rocks based on the convolutional neural network and logging curves – A case study of Pinghu Formation in Xihu Sag
- A method for fast detection of wind farms from remote sensing images using deep learning and geospatial analysis
- Spatial distribution and driving factors of karst rocky desertification in Southwest China based on GIS and geodetector
- Physicochemical and mineralogical composition studies of clays from Share and Tshonga areas, Northern Bida Basin, Nigeria: Implications for Geophagia
- Geochemical sedimentary records of eutrophication and environmental change in Chaohu Lake, East China
- Research progress of freeze–thaw rock using bibliometric analysis
- Mixed irrigation affects the composition and diversity of the soil bacterial community
- Examining the swelling potential of cohesive soils with high plasticity according to their index properties using GIS
- Geological genesis and identification of high-porosity and low-permeability sandstones in the Cretaceous Bashkirchik Formation, northern Tarim Basin
- Usability of PPGIS tools exemplified by geodiscussion – a tool for public participation in shaping public space
- Efficient development technology of Upper Paleozoic Lower Shihezi tight sandstone gas reservoir in northeastern Ordos Basin
- Assessment of soil resources of agricultural landscapes in Turkestan region of the Republic of Kazakhstan based on agrochemical indexes
- Evaluating the impact of DEM interpolation algorithms on relief index for soil resource management
- Petrogenetic relationship between plutonic and subvolcanic rocks in the Jurassic Shuikoushan complex, South China
- A novel workflow for shale lithology identification – A case study in the Gulong Depression, Songliao Basin, China
- Characteristics and main controlling factors of dolomite reservoirs in Fei-3 Member of Feixianguan Formation of Lower Triassic, Puguang area
- Impact of high-speed railway network on county-level accessibility and economic linkage in Jiangxi Province, China: A spatio-temporal data analysis
- Estimation model of wild fractional vegetation cover based on RGB vegetation index and its application
- Lithofacies, petrography, and geochemistry of the Lamphun oceanic plate stratigraphy: As a record of the subduction history of Paleo-Tethys in Chiang Mai-Chiang Rai Suture Zone of Thailand
- Structural features and tectonic activity of the Weihe Fault, central China
- Application of the wavelet transform and Hilbert–Huang transform in stratigraphic sequence division of Jurassic Shaximiao Formation in Southwest Sichuan Basin
- Structural detachment influences the shale gas preservation in the Wufeng-Longmaxi Formation, Northern Guizhou Province
- Distribution law of Chang 7 Member tight oil in the western Ordos Basin based on geological, logging and numerical simulation techniques
- Evaluation of alteration in the geothermal province west of Cappadocia, Türkiye: Mineralogical, petrographical, geochemical, and remote sensing data
- Numerical modeling of site response at large strains with simplified nonlinear models: Application to Lotung seismic array
- Quantitative characterization of granite failure intensity under dynamic disturbance from energy standpoint
- Characteristics of debris flow dynamics and prediction of the hazardous area in Bangou Village, Yanqing District, Beijing, China
- Rockfall mapping and susceptibility evaluation based on UAV high-resolution imagery and support vector machine method
- Statistical comparison analysis of different real-time kinematic methods for the development of photogrammetric products: CORS-RTK, CORS-RTK + PPK, RTK-DRTK2, and RTK + DRTK2 + GCP
- Hydrogeological mapping of fracture networks using earth observation data to improve rainfall–runoff modeling in arid mountains, Saudi Arabia
- Petrography and geochemistry of pegmatite and leucogranite of Ntega-Marangara area, Burundi, in relation to rare metal mineralisation
- Prediction of formation fracture pressure based on reinforcement learning and XGBoost
- Hazard zonation for potential earthquake-induced landslide in the eastern East Kunlun fault zone
- Monitoring water infiltration in multiple layers of sandstone coal mining model with cracks using ERT
- Study of the patterns of ice lake variation and the factors influencing these changes in the western Nyingchi area
- Productive conservation at the landslide prone area under the threat of rapid land cover changes
- Sedimentary processes and patterns in deposits corresponding to freshwater lake-facies of hyperpycnal flow – An experimental study based on flume depositional simulations
- Study on time-dependent injectability evaluation of mudstone considering the self-healing effect
- Detection of objects with diverse geometric shapes in GPR images using deep-learning methods
- Behavior of trace metals in sedimentary cores from marine and lacustrine environments in Algeria
- Spatiotemporal variation pattern and spatial coupling relationship between NDVI and LST in Mu Us Sandy Land
- Formation mechanism and oil-bearing properties of gravity flow sand body of Chang 63 sub-member of Yanchang Formation in Huaqing area, Ordos Basin
- Diagenesis of marine-continental transitional shale from the Upper Permian Longtan Formation in southern Sichuan Basin, China
- Vertical high-velocity structures and seismic activity in western Shandong Rise, China: Case study inspired by double-difference seismic tomography
- Spatial coupling relationship between metamorphic core complex and gold deposits: Constraints from geophysical electromagnetics
- Disparities in the geospatial allocation of public facilities from the perspective of living circles
- Research on spatial correlation structure of war heritage based on field theory. A case study of Jinzhai County, China
- Formation mechanisms of Qiaoba-Zhongdu Danxia landforms in southwestern Sichuan Province, China
- Magnetic data interpretation: Implication for structure and hydrocarbon potentiality at Delta Wadi Diit, Southeastern Egypt
- Deeply buried clastic rock diagenesis evolution mechanism of Dongdaohaizi sag in the center of Junggar fault basin, Northwest China
- Application of LS-RAPID to simulate the motion of two contrasting landslides triggered by earthquakes
- The new insight of tectonic setting in Sunda–Banda transition zone using tomography seismic. Case study: 7.1 M deep earthquake 29 August 2023
- The critical role of c and φ in ensuring stability: A study on rockfill dams
- Evidence of late quaternary activity of the Weining-Shuicheng Fault in Guizhou, China
- Extreme hydroclimatic events and response of vegetation in the eastern QTP since 10 ka
- Spatial–temporal effect of sea–land gradient on landscape pattern and ecological risk in the coastal zone: A case study of Dalian City
- Study on the influence mechanism of land use on carbon storage under multiple scenarios: A case study of Wenzhou
- A new method for identifying reservoir fluid properties based on well logging data: A case study from PL block of Bohai Bay Basin, North China
- Comparison between thermal models across the Middle Magdalena Valley, Eastern Cordillera, and Eastern Llanos basins in Colombia
- Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts
- Chlorite-induced porosity evolution in multi-source tight sandstone reservoirs: A case study of the Shaximiao Formation in western Sichuan Basin
- Predicting stability factors for rotational failures in earth slopes and embankments using artificial intelligence techniques
- Origin of Late Cretaceous A-type granitoids in South China: Response to the rollback and retreat of the Paleo-Pacific plate
- Modification of dolomitization on reservoir spaces in reef–shoal complex: A case study of Permian Changxing Formation, Sichuan Basin, SW China
- Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration
- Rock physics model for deep coal-bed methane reservoir based on equivalent medium theory: A case study of Carboniferous-Permian in Eastern Ordos Basin
- Enhancing the total-field magnetic anomaly using the normalized source strength
- Shear wave velocity profiling of Riyadh City, Saudi Arabia, utilizing the multi-channel analysis of surface waves method
- Effect of coal facies on pore structure heterogeneity of coal measures: Quantitative characterization and comparative study
- Inversion method of organic matter content of different types of soils in black soil area based on hyperspectral indices
- Detection of seepage zones in artificial levees: A case study at the Körös River, Hungary
- Tight sandstone fluid detection technology based on multi-wave seismic data
- Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
- Influence of pore structure characteristics on the Permian Shan-1 reservoir in Longdong, Southwest Ordos Basin, China
- Study on sedimentary model of Shanxi Formation – Lower Shihezi Formation in Da 17 well area of Daniudi gas field, Ordos Basin
- Multi-scenario territorial spatial simulation and dynamic changes: A case study of Jilin Province in China from 1985 to 2030
- Review Articles
- Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
- Prediction and assessment of meteorological drought in southwest China using long short-term memory model
- Communication
- Essential questions in earth and geosciences according to large language models
- Erratum
- Erratum to “Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan”
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part I
- Spatial-temporal and trend analysis of traffic accidents in AP Vojvodina (North Serbia)
- Exploring environmental awareness, knowledge, and safety: A comparative study among students in Montenegro and North Macedonia
- Determinants influencing tourists’ willingness to visit Türkiye – Impact of earthquake hazards on Serbian visitors’ preferences
- Application of remote sensing in monitoring land degradation: A case study of Stanari municipality (Bosnia and Herzegovina)
- Optimizing agricultural land use: A GIS-based assessment of suitability in the Sana River Basin, Bosnia and Herzegovina
- Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index
- Analysis of the intensity of erosive processes and state of vegetation cover in the zone of influence of the Kolubara Mining Basin
- GIS-based spatial modeling of landslide susceptibility using BWM-LSI: A case study – city of Smederevo (Serbia)
- Geospatial modeling of wildfire susceptibility on a national scale in Montenegro: A comparative evaluation of F-AHP and FR methodologies
- Geosite assessment as the first step for the development of canyoning activities in North Montenegro
- Urban geoheritage and degradation risk assessment of the Sokograd fortress (Sokobanja, Eastern Serbia)
- Multi-hazard modeling of erosion and landslide susceptibility at the national scale in the example of North Macedonia
- Understanding seismic hazard resilience in Montenegro: A qualitative analysis of community preparedness and response capabilities
- Forest soil CO2 emission in Quercus robur level II monitoring site
- Characterization of glomalin proteins in soil: A potential indicator of erosion intensity
- Power of Terroir: Case study of Grašac at the Fruška Gora wine region (North Serbia)
- Special Issue: Geospatial and Environmental Dynamics - Part I
- Qualitative insights into cultural heritage protection in Serbia: Addressing legal and institutional gaps for disaster risk resilience