2.2.1. Hoek-Brown Guidelines
The Hoek-Brown criterion is an empirical guideline for determining the mechanical parameters of a rock mass and includes the GSI geostrength index and the rock disturbance coefficient D.
The expression for the Hoek-Brown empirical criterion [
35] is:
where
σ1 and
σ3 are the maximum and minimum principal stresses,
σci is the uniaxial compressive strength of the rock mass, and
mb,
s, and
a are the semi-empirical parameters of rock properties as a function of the Geological Strength Index GSI [
36]:
In the formula, Jcond89 is the state of joints, RQD is the quality of rock, GSI is the geological strength index, the three take values in the range of 5~100; mi is the rock material constant, obtained from the triaxial compression test of intact rock, can also be determined according to the type of rock, the structure, take the value of the range of 5~40; D is the weakening factor for the consideration of the rock body by anthropogenic or natural factors of perturbation, take the value of the range of 0~1.
1) Determination of modulus of elasticity
The modulus of elasticity is an important parameter describing the strength of a material, and the modulus of elasticity
Em (GPa) of a rock is calculated as:
2) Determination of shear strength parameters
The shear strength parameters are cohesion
c and friction angle
φ. The expressions for the equivalent cohesion
c′ and equivalent friction angle
φ′ of the rock adopted by the Hoek-Brown criterion are, respectively:
where
=
/
σci , and for deep tunnels
can be determined by the following equation:
where
γ is the bulk weight of the rock mass;
H is the burial depth of the tunnel, and when the horizontal stress is higher than the vertical stress,
γH in Eq. (10) is replaced by the value of the horizontal stress;
is the strength of the rock mass, which is calculated by the formula:
(3) Disturbance factor of rock mass for tunneling D
The disturbance factor for the rock mass is usually taken empirically, as shown in
Table 1.
2.2.2. Determination of Rock Reduction Parameters
1)Hoek-Brown criterion parameterization
(1)GSI value determination
The Hoek-Brown criterion parameters were determined on the basis of the distribution profiles of rock layers and surrounding rock grades in the new tunnels, the overtopping geological forecast, and the observation information of the palm face, combined with the GSI index map proposed by Hoke et al [
36].
a.Rock layer and surrounding rock grading section
The new Wanshoushan Tunnel is a double-line highway tunnel, the left line intersects with Hurong Railway Tunnel at K3+674.943 (
Figure 2 L
0), and the right line intersects with Hurong Railway Tunnel at YK3+694.291 (
Figure 3 R
0). The 60m before and after the intersection point of the new highway tunnel is the excavation sensitive area [
34], as shown in
Figure 2-2. Preliminarily, the excavation sensitive area is determined as Class IV surrounding rock. Typical cross-sections of 60m and 85m before and after the tunnel intersection are extracted for analysis, the left line: L1 section K3+590, L2 section K3+615, L3 section K3+735, L4 section K3+760, and the right line: R1 section YK3+609, R2 section YK3+634, R3 section YK3+754, R4 section YK3+779.
b.Over-advanced geological forecast
The equipment used for advanced geological forecasting is SRI-20 geological radar combined with 100MHz antenna, as shown in
Figure 4. The geological forecast line is 12m long and distributed in the shape of a zigzag at the bottom of the upper step of the palm face, 1.2m away from the height of the lower step (
Figure 5).
c. Left line palm surface observation and radar data analysis
The surrounding rocks of L1 and L2 sections are mainly medium-weathered grayish-white malmstone, with good integrity and interlayer combination, undeveloped joints and fissures, and a dry palm surface. a small amount of mudstone locally exists in L1, with medium-thickness bedding, and thick bedding is dominant in L2.
The surrounding rock of L3 section is mainly mudstone, which is soft rock. The rock body is relatively broken, mainly in thin layers, the combination between rock layers is general, joints and fissures are developed, strong weathering is dominant, and the palm surface is dry.
The surrounding rocks in section L4 are mainly mudstone, and there are obvious malmstone and mudstone interlayers within 2m above the upper step, of which mudstone is soft rock and malmstone is hard rock. The rock body is more complete, the combination between the rock layers is general, the joints and fissures are developed, medium weathering is dominant, and the palm surface is drier.
The radar reflection signals of L1 and L2 sections are strong, and the frequency change of electromagnetic wave signals is general and continuous in the same direction, L1 is dominated by medium-low frequency signals, and L2 is dominated by medium-high frequency signals. Combined with the condition of the palm surface of the section, it is concluded that the 0~25m section in front of the L1 and L2 section is mainly malmstone, which belongs to the harder rock, the joints and fissures are not developed, and the integrity of the rock body is better, and it is the IV level of preferred surrounding rock.
L3 section radar reflection signal is strong, electromagnetic wave signal frequency change is general, mainly in the middle and high frequency signal, isotropic axis intermittent, local continuous, no obvious shock wave signal. Combined with the situation of palm surface in L3 section, it is concluded that mudstone is dominated in the range of 0~25m in front of L3 section, which is soft rock, with joints and fissures developed, and the integrity of surrounding rock is general, and there are weak and soft surrounding rock segments in the local area, and it is a class IV deviation surrounding rock.
The radar reflection signal of L4 section is strong, and the frequency change of electromagnetic wave signal is general, dominated by homogeneous medium-low frequency signal, with continuous isotropic axis and no obvious shock wave signal. Combined with the situation of the palm face of L4 section, it is concluded that mudstone is dominant in the range of 0~25m in front of L4 section, and there may be malmstone and mudstone interbedding in the local area, of which mudstone is soft rock and malmstone is harder rock, with joints and fissures developed, and the integrity of surrounding rock is general, and it is class IV surrounding rock.
d.Observation and radar data analysis of the right line palm surface
The surrounding rocks in section R1 are mainly gray-white malmstone, the rock body is complete, mainly medium-thick laminated, the combination between the rock layers is good, the joints and fissures are not developed, mainly medium weathering, and the palm face is dry.
The surrounding rocks in section R2 are mainly malmstone, mixed with mudstone, malmstone is soft rock, mudstone is soft rock, and there is obvious interlayer in the middle of the palm face. The surrounding rocks are mainly medium-thick bedded, the integrity of the rock body is general, the combination between the rock layers is general, the joints and fissures are developed, strong weathering is dominant, and the palm surface is dry.
The surrounding rocks in section R3 are mainly mudstone and malmstone, mudstone is soft rock and malmstone is hard rock. The rock body is more broken, mainly in thin layers, and the combination between the rock layers is poor.
R4 section is mainly surrounded by mudstone, which is soft rock, surrounded by thin layer, the integrity of rock body is general, and the combination between rock layers is general~better.R3 and R4 sections have developed joints and fissures, which are mainly strongly weathered, and the palm surface is dry.
The radar reflection signal is stronger in section R1 and weaker in section R2.R1 and R2 electromagnetic wave signal frequency change is general, mainly in low frequency signal, isotropic axis intermittent, combined with the section palm surface of the situation of R1 and R2 section in front of the 0~25m section to malmstone is dominated by the malmstone, mixed with mudstone, malmstone belongs to the softer rock, mudstone belongs to the soft rock. The joints and fissures are developed, and the rock body integrity is general, which is class IV surrounding rock.
R3 section radar reflection signal is strong, the electromagnetic wave signal frequency change is general, mainly in the middle and high frequency signal, the same direction axis is locally continuous, locally intermittent, the amplitude is general. Combined with the situation of R3 section palm face, it is concluded that 0~25m range in front of R3 section is dominated by mudstone and malmstone, mudstone belongs to soft rock, malmstone belongs to hard rock, joints and fissures are developed in the range of 0~10m in front of palm face, and the integrity of peripheral rock is general, and it is the peripheral rock of IV level deviation.
The radar reflection signal of R4 section is strong, and the frequency change of electromagnetic wave signal is general, dominated by medium and high frequency signal, with the same direction axis continuous, without obvious shock wave signal. Combined with the situation of R4 section palm face, it is concluded that the range of 0~25m in front of R4 section is dominated by mudstone, which is soft rock, with undeveloped joints and fissures, and the integrity of surrounding rock is general, and it is a class IV deviation surrounding rock.
The photo of the new tunnel palm face and the result of the analysis of the overtopping geological prediction radar data are in good agreement with the grading profile of the rock layers and the surrounding rocks. Therefore, it is finally determined that the malmstone layer of the cross-tunnel project (assuming that the grading of the surrounding rocks of the existing tunnels is the same as that of the new tunnels) is a Class IV preferred surrounding rock and the mudstone layer is a Class IV deviated surrounding rock, and at the same time, with reference to the GSI index diagram (
Figure 22), it is determined that the malmstone and mudstone layers have a GSI value of 55 and 45.
(2)Determination of rock integrity coefficient mi
Based on the palm face observation and overtopping geological forecast information, the integrity coefficient of rock
mi was determined by rock type and structure[
36] (
Table 2), and the integrity coefficients of malmstone and mudstone formations of the cross-tunneling project were determined to be 21 and 9.
(3) Determination of uniaxial compressive strength σci of rocks
Test uniaxial compression test is carried out to determine the uniaxial compressive strength of malmstone and mudstone of cross tunnel project as 8.9 MPa and 3.84 MPa respectively.
(4) Determination of disturbance coefficient D
Based on the disturbance situation of the field tunnel[
34], referring to the rock disturbance coefficient value chart (
Table 1), it is determined that the disturbance coefficient of the area affected by blasting and excavation of the cross-tunnel project is 0.5, that of the area affected by static excavation is 0, that of the area affected by the train dynamic load is 0.2, and that of the area overlapping the blasting load and the train dynamic load is 0.7.
(5) Determination of rock mass related parameters for cross-tunneling project
The average depth of the new tunnel is 460m, the average depth of the existing tunnel is 420m, the average depth of the overlapping area is 445m, and the average weight of the overlying rock layer takes the average value of the weight of malmstone and mudstone to be 23.51kN/m
3. The values of GSI,
mi,
σci,
D,
γ, and
H will be brought into the corresponding formulas, which will result in the values of the relevant parameters of the rock body in the area affected by the cross-tunneling project, and the details are shown in
Table 3.
2) Determination of mechanical parameters of rock body
The values of the relevant parameters in
Table 3 of the rock mass and literature [
34] were brought into the previous equations to derive the parameters of elastic modulus, equivalent cohesion, equivalent internal friction angle and Poisson's ratio for different influence regions [
37], which are detailed in
Table 4.