1. Introduction
Open-pit bench blasting is widely employed in mining engineering due to its cost effectiveness and high efficiency. However, drilling and blasting inevitably generate harmful effects [
1,
2], and the effect of blast-induced vibration on the stability of buildings (structures) within a specific range is the most prominent [
3,
4]. In particular, when the open-pit mining areas are adjacent to underground mining zones, the effects of blast-induced vibration pose a severe threat to the stability and safety of adjacent underground large-section rectangular coal roadways, such as wall caving, crack development in the surrounding rock, roof collapse, etc. Therefore, the dynamic response of large-section rectangular coal roadway surrounding rock under the effect of blast-induced vibration should be investigated in open-pit mining, and an accurate model for predicting the peak particle velocity (PPV) of the surrounding rock should be established. It is of great engineering significance for preventing damage to large-section rectangular coal roadways caused by intense vibrations resulting from large-charge, deep-hole bench blasting in open-pit mines, as well as ensuring their structural stability.
The PPV is a primary metric for assessing the strength of blast-induced vibrations. It is a key parameter in blast vibration safety standards [
5,
6]. Therefore, it is often used as a control criterion for blast vibration.
In terms of open-pit blasting, Duvall and Fogelson [
7] investigated the attenuation of blasting seismic waves and established seismic standards for various buildings. The USBM investigators Ambraseys and Hendron [
8] advised the actual distance to be divided by the cube root of the charge weight. Bilgin et al. [
9] proposed an equation by adding a burden parameter to classical PPV prediction models. Rai and Singh [
10] proposed a PPV prediction equation considering an inelastic attenuation factor and analyzed its calculation results in comparison with other vibration prediction equations for the same dataset. The analysis shows that this prediction formula can be effectively used for calculating the safe charge per delay more precisely. Ak and Konuk [
11] investigated the impacts of discontinuity frequency on the propagation of blast-induced vibration in bench blasting and established the relationship between the scaled distance and discontinuity frequency with the PPV. Y. Yan et al. [
12] summarized the influential parameters on blast-induced ground vibrations and evaluated the free face, maximum charge per delay, distance from the blasting source to the monitored point, and geological conditions, confirming their influence in predicting the PPV. Khandelwal et al. [
13] analyzed various blasting design parameters on predicting the PPV and proposed a new empirical equations based on dimensional analysis. It comprehensively reflected the influence of parameters such as the Young’s modulus of rock mass, powder factor, depth and hole diameter, spacing, burden, and charge length on the attenuation law of blast-induced vibration. W. M. Yan et al. [
14] found that the influential parameters and empirical equations for predicting the PPV were uncertain and proposed using the Bayesian technique and Monte Carlo simulation to predict the PPV. This method could offer practicing engineers confidence intervals when the equation is used to estimate a blast-induced vibration. Based on the scaled distance concept used for inelastic attenuation factor, Simangunsong and Wahyudi [
15] analyzed the effect of a bedding plane on the prediction of blast-induced ground vibration in open-pit coal mines. Based on the analysis results, the relationship between the incident angle, the number of coal layers, and the PPV was established. Yilmaz [
16] proposed a new equation for predicting the PPV, for which the coefficient of determination of regression results was high, indicating the correlation between the scaled distance and the PPV with inelastic attenuation. Kumar et al. [
17] proposed an empirical equation for predicting the PPV by considering the effects of rock mechanical and geological properties, like the unit weight, rock quality designation (RQD), geological strength index (GSI), and uniaxial compressive strength (UCS). Chen et al. [
18] investigated the influence of the cylindrical charge length on blast-induced vibration based on elastic–plastic theory and provided a new equation for predicting the PPV considering the characteristics of cylindrical charge length. Murmu et al. [
19] proposed two empirical equations, one considering the overburden and the other without it. Compared with the regression results of two empirical equations, the results showed that overburden did not significantly affect PPV. Yin et al. [
20] investigated different rock masses on the attenuation characteristics of blast-induced vibration, The results indicated that the development degree of rock mass joints affected the attenuation rate of the PPV. It indicated that the more joints there are, the higher the attenuation rate of the PPV. A modified equation for predicting PPV was developed by considering the joint number in the rock mass. Deng et al. [
21] derived the empirical equation for predicting PPV, which was modified for multi-hole blasting based on stress wave propagation theory. The proposed model could adequately reflect the propagation of PPV under multi-hole blasting.
In terms of underground blasting, Nan Jiang et al. [
22] investigated the blast-induced vibration attenuation of the slope subjected to underground mining and analyzed the distribution characteristics of PPV. Meanwhile, a PPV prediction model suitable for open-pit mine slopes subjected to underground mining considering the mining depth and elevation was proposed. Nan Jiang et al. [
23] investigated the impact of subway excavation on adjacent buried gas pipelines, and a mathematical model was established to describe the attenuation of the PPV with respect to the depth of tunnel blasting. Wang et al. [
24], based on the diffraction and reflection amplification effects of blast-induced vibration around tunnels, calculated the possible minimum diffraction distance of blast-induced vibration around the rock tunnels and improved the scaled distance (SD) of the empirical equations to predict the PPV on adjacent tunnel sections. This equation efficiently enhanced the accuracy of predicting the PPV. W. Li et al. [
25] compared several empirical equations for predicting the PPV of the adjacent tunnel surrounding rock based on the rock strength index (GSI). The improved equations could be adopted to predict the PPV for complex geological conditions.
In the field of machine learning and artificial intelligence, and with its rapid development [
26,
27], these methods are widely used in predicting blast-induced vibration and show excellent applicability.
Many research studies have been carried out on the effect of open-pit bench blasting and the corresponding influence of blast-induced vibration on the dynamic response of underground roadways. Litwiniszyn J [
28] carried out a theoretical investigation into dynamic instability in underground roadways caused by blast-induced stress waves. It was found that a rarefaction stress wave and a jump-like change in the state of stress in the surrounding rock are generated when the surrounding rock reaches the instability condition. Within the interval of the jump-like change in stress, the skeleton of the surrounding rock is destroyed, and an outburst is initiated. Singh et al. [
29,
30] analyzed the dynamic response of blast-induced vibration on the top plate, pillar, and bottom plate of an adjacent roadway in open-pit blasting and determined the safety thresholds for the vibration of the underground roadway surrounding rocks. Duan et al. [
31] evaluated the stability of open-pit bench blast seismic waves on the surrounding rocks and ancillary structures of underground roadways. However, the influence of the roadway cavity and the dynamics response of the relative position on the evolution of the surrounding rock and the accuracy of predicting the PPV have not been considered in previous studies.
Although the research on blast-induced vibration PPV control and prediction has been fully developed and applied, the influence of the differences in reflection and stacking effects of blasting stress waves on the coal roadway surrounding rock on each side (i.e., “the cavity effect”), as well as the relative position of the blasting-induced dynamic disturbance, on stress evolution and the accuracy of PPV prediction in large-section rectangular coal roadway surrounding rock has not yet been thoroughly investigated. Therefore, in this paper, the vibration response of roadway surrounding rock was carried out using stress wave propagation theory and conservation laws of wave-front momentum. Then, the dynamic response of the large-section rectangular coal roadway surrounding rock was analyzed under varying blast source distances and relative angle (i.e., , the relative angle between the position of the open-pit bench blasting with the underground coal roadway) conditions using finite element (FE) analysis. Finally, based on the analysis of the cavity effect in the vibration response of large-section coal roadway surrounding rock, a PPV prediction model incorporating the relative angle () as one of the key influencing factors was developed, which aimed to significantly improve adaptability and prediction accuracy, providing a more precise tool for predicting the vibration response of the large-section coal roadway surrounding rock. This research provides the theory for the precise prevention of underground large-section coal roadway dynamic instability failures under vibrations due to open-pit bench blasting.
2. Vibrating Equations for the Adjacent Roadway in Open-Pit Bench Blasting
The open-pit bench blasting load enhances the dynamic response of the underground roadway surrounding rock, and the stress in the surrounding rock is redistributed under the action of blast-induced and surface reflection stress waves. When stress intensity is greater than the dynamic strength threshold of the rock mass, it promotes crack propagation and expansion in the surrounding rock, deteriorating the properties and reducing the bearing capacity of the surrounding rock, thereby inducing sudden instability in the surrounding rock. In open-pit bench blasting, underground roadways are mainly affected by blast-induced stress waves and reflected stress waves from the surface. As shown in
Figure 1, after the blast-induced stress wave is reflected on the surface, it generates reflected P-waves and S-waves. Meanwhile, the incident wave generates reflected P-waves and S-waves on the free surface of the roadway surrounding rock.
The calculations were further simplified by adopting the following steps:
- (1)
The cylindrical charge was simplified to spherical charge, while only P-waves with a constant excitation frequency were considered; this assumption was suitable for the preliminary approximate analysis, but it may ignore the different propagation characteristics of the cylindrical charge in the axial and radial directions.
- (2)
The rock mass was assumed to be a homogeneous and isotropic linear elastomer.
- (3)
The compressive stress was defined to be positive.
In the analysis, the case of blast-induced stress waves and surface-reflected stress waves acting on the free face of the roadway surrounding rock was considered a special case of stress wave propagation in joints [
32], i.e., the rock on the other side of the joints was replaced by air (wave impedance is 0). This was based on the theory of stress wave propagation and the theorem of momentum conservation in front of the wave, combined with the time-domain recursive method [
32,
33,
34], to carry out the derivation of vibrating equations for the surrounding rock of cavity roadway under the action of blasting stress waves and surface-reflected stress waves.
2.1. Interaction of the Blast Stress Wave with the Surface
As illustrated in
Figure 2a, when an incident P-wave propagates to a free face, a tiny element ABC consists of AB, AC, and BC, where AB is the free face of the surface, BC and AC are the wave beam and the wave front of the P-wave, respectively, and is
the angle of incidence. The tiny element of the reflected P-wave interacting with the rock is ABE, BE is the wave front of the reflected P-wave, and AE is the wave beam of the reflected P-wave. According to Snell’s law [
32], the incidence and the reflection angles of the P-wave are equal, so the angle of the reflected P-wave is also
, as shown in
Figure 2b. Similarly, the tiny element of the reflected S-wave interacting with the rock is ABF, and BF, AF, and
are the wave front, wave beam, and the angle of the reflected S-wave, respectively, as shown in
Figure 2c.
Approximating the current model as a one-dimensional strain plane wave problem, assuming that the transverse dimension of the free surface is infinitely large, the plane wave can be regarded as a one-dimensional strain wave for analysis, and combined with one-dimensional strain elastic wave theory, the stress on the BC is determined to be equal to
[
33,
35,
36], where
is the normal stress of the wave front of the incident P-wave, and
denotes the Poisson’s ratio of the rock.
Without considering gravity, the stress for the tiny elements ABC of the surface is shown in
Figure 2a, where
and
are the direct and shear stresses of the rock on the left side of the free face, respectively. From the force equilibrium condition of tiny elements, the stresses in the vertical direction and radial direction of the free surface AB on the element ABC must satisfy Equations (1) and (2) [
34].
In the vertical direction of the free surface AB:
In the radial direction of the free surface AB:
According to the Snell’s law [
34]:
where
and
are the velocities of the P-wave and S-wave in intact rock, respectively.
The expression for
considering
and
can be obtained and substituted into Equations (1) and (2) and can be expressed as Equation (4).
Similarly, under the influence of reflected P-waves and reflected S-waves, the stresses
and
on the tiny elements ABE and ABF on the free face can be expressed as Equations (5) and (6).
Then, the total stress on the free face can be expressed as Equations (7) and (8).
On the boundary of the free surface, the stresses satisfied the conditions of
and
. Based on Equations (7) and (8), the reflection stresses of the surface free boundary can be expressed as Equations (9)–(11).
2.2. Interaction of Blasting Stress Wave and Surface-Reflected Wave with Roadway Surrounding Rock
Similar to stress waves interacting with the ground surface, the force state on tiny elements of the roadway surrounding rock acted by the incident P-wave and the surface-reflected wave is shown in
Figure 3, respectively.
In
Figure 3,
and
denote the normal stresses of the incident P-wave and reflected P-waves on their wave fronts under blasting stress, respectively;
denotes the shear stresses of the reflected S-waves on the wave fronts under blasting stress.
and
denote the normal stress of P-waves and the shear stress of S-waves reflected from the surface, respectively.
is the angle of incidence.
For the elements
,
,
,
, and
on the free face of the roadway surrounding rock in
Figure 3, the stresses
and
can be expressed as Equations (12)–(16):
where
is the angle of the incident P-wave by the blasting stress, which is equal to the angle of the reflected P-wave;
is the angle of the reflected S-wave by the blasting stress;
is the angle of incident P-waves reflected from the surface; and
is the angle of S-waves reflected from the surface.
According to the law of conservation of momentum in the wave front, , , , , and , where and are the particle velocities of the incident and reflected P-waves of blasting stress, respectively; is the particle velocity of the reflected P-waves of surface-reflected waves; and and are the particle velocities of the reflected S-waves of blasting stress waves and surface reflection waves, respectively. Hence, the correlation between the stresses on the free face of the roadway surrounding rock and the particle velocities was established. We define and , where is the density of the intact rock; the meanings of and are the same as above.
According to the law of momentum conservation at the wave front, the time interval between the incident stress wave and the reflected stress wave is negligible. As a result, both the incident and reflected stress waves act simultaneously on the roadway surrounding rock. Thus, the sum of stresses at the units on the free face of the roadway surrounding rock can be expressed as Equations (17) and (18).
On the free face of the roadway surrounding rock, the stresses still satisfy
and
. Equations (17) and (18) can be expressed in matrix form as Equation (19), whereas the individual matrices are given by Equations (20)–(22).
The normal components of the velocities on the free face of the roadway surrounding rock can be expressed as Equation (23).
The tangential components of the velocities on the free face of the roadway surrounding rock can be expressed as Equation (24).
Equations (23) and (24) can be expressed in matrix form, as given in Equations (25)–(29).
Equation (26) can be expressed as the vibration equation on the roadway surrounding rock induced by open-pit bench blasting. It is concluded that the particle velocity on the roadway surrounding rock is related to the surrounding rock density, the wave velocity of P- and S-waves, and the angles of incidence and reflection. It confirmed that for the same geological conditions, rock density, wave velocity, and distance between the blasting area and the roadway, the incidence angle of the stress wave determines the characteristics of the dynamic response at different locations of the roadway surrounding rock, leading to disparities in the particle velocity at various locations of the roadway surrounding rock under the bench blasting.
4. Numerical Results
4.1. Analysis of the Cavity Effect on the Roadway Surrounding Rock
Numerical simulations of the dynamic disturbance on the roadway surrounding rock in open-pit bench blasting with different distances and bench heights were carried out. In order to investigate the influence of bench height on the cavity effect in open-pit bench blasting, the stress clouds of roadway surrounding rock in different blasting locations were produced and are shown in
Figure 9.
In order to further analyze the stress wave propagation in the roadway surrounding rock, the blasting source at the right, upper left, and top of the roadway were simulated. The resulting stress maps are shown in
Figure 9a–d,
Figure 9e–h, and
Figure 9i–l, respectively. It is concluded that the stress wave propagates to the free face of the roadway surrounding rock, and the stress wave is reflected at the free interface of the roadway due to the influence of the free face, with the unloading wave following the incident pressure loading wave and the surface-reflected stress wave to produce complex stress wave superposition action at the free interface of the roadway surrounding rock. Furthermore, the face-explosion side of the roadway surrounding rock is the main influence area under the repeated tensile and compressive effects of the stress wave. In the back-explosion side of the roadway, stress wave wave fronts move in opposite directions on both sides and converge in the middle of the back-explosion side. The stress wave effect was enhanced, but the dynamic response on the back blast side of the surrounding rock was smaller.
It is also deduced that the stress wave propagation direction is affected by the cavity roadway, and the stress wave propagates around the roadway to the undisturbed area. The disparity in the incidence angles of the stress wave wave front at each mass point of the roadway surrounding rock leads to the difference among the effects of the reflection and superposition stress waves at each mass point. Meanwhile, the effects cause different stress states at the mass points, indicating that the difference in stress state is related to the angle of the incident stress wave on the free face of the roadway surrounding rock. The difference in blast loading on each side of the rectangular roadway surrounding rock indicates the cavity effect of the roadway on the propagation of the blasting stress wave around the rectangular roadway.
It is seen in
Figure 9 that when the location of the blasting source was changed from the same bench to the top of the roadway surrounding rock, the stress wave intensity reaching the roadway was reduced. Meanwhile, the relative angle of the stress wave wave front acting on the roadway was also changed. It led to a change in the reflected wave angle on the roadway surrounding rock and the regional location of the reflection and superposition effect of stress wave on the free face of the roadway rock, causing significant disparities in the stress distribution with the roadway surrounding rock under different levels of bench blasting. It is demonstrated that the relative angle (
) is one of the critical factors affecting the stress evolution and dynamic damage of the roadway surrounding rock.
4.2. Particle Velocity Distribution on the Rectangular Roadway Surrounding Rock
Equally spaced units along the contour of the roadway surrounding rock were selected to monitor the PPV. The selected units are shown in
Figure 10. To investigate the radial and tangential vibration distribution law, different distances from the blasting source to the selected units and benches were selected. The variation curves of the surrounding rock’s PPV are presented in
Figure 11.
Figure 11 shows that the PPV of the profile surface of the roadway surrounding rock is significantly different. The PPV of the face-explosion side affected by the explosion was the largest. Compared with the PPV of the face-explosion side, the PPV of the back-explosion side was significantly weak. However, the seismic wave converged in the middle area of the back-explosion side, and the vibration strength of the surrounding rock appeared to be a sudden leap.
Since , for the same rock properties, the particle velocity of the surrounding rock is proportional to the dynamic stress. By the effect of roadway cavity, roadway rock free surface, and blasting seismic wave propagation and attenuation, the relative angle of the stress wave incident on the free face of the roadway surrounding rock mass is different, leading to varying particle velocities of each mass point of the roadway surrounding rock caused by the incident, reflection, and superposition effects of the stress wave. The energy of the blasting stress wave is rapidly attenuated during propagation. Therefore, the PPV of the roadway surrounding rock on each side is significantly different. This reflects the significant correlation between the PPV of the roadway surrounding rock and the incident angle of the stress wave.
The comparison of the PPV of the roadway surrounding rock under different levels of bench blasting revealed that the blasting position at the same bench of the roadway had the greatest impact on the PPV of the roadway surrounding rock, followed by top blasting, whereas side blasting resulted in the smallest PPV of the surrounding rock.
As the stress wave propagated from the rock medium to the coal medium, an unloading effect occurred at the stratified interface of rock, leading to further attenuation of the stress wave wave front. Additionally, the unloading intensity of the reflected and transmitted waves was influenced by the incident angle of the stress wave at the stratified interface. Above all, it indicated that the change in relative angle (θ) led to different stress intensities acting directly on the surrounding rock of the roadway, resulting in disparities in the PPV of the roadway surrounding rock. It reflected that the relative angle (θ) was a critical factor governing the vibration intensity of the surrounding rock on each side of the roadway.
4.3. Influence of Distance on the Cavity Effect
Figure 12a shows the maximum ratio of the PPV between the face-explosion side and the back-explosion side of the roadway as 5.06 when the distance from the blasting source to the roadway was 120 m. When the distance from the blasting source to the roadway was gradually reduced to 36 m, the ratio of the PPV was progressively increased to 8.13, and the difference in the PPV of the roadway surrounding rock was relatively significant. As the distance decreases, the cavity effect promotes a considerable increase in the ratio of the PPV of the roadway surrounding rock on each side of the roadway. From
Figure 12b,c, the same conclusion is obtained for the cavity effect under the bench blasting at different locations.
In summary, the cavity effect changes the stress wave propagation in the roadway surrounding rock. The change in the relative angle (θ) between the blasting source and the roadway promotes an angle change in the stress wave wave front acting on the roadway surrounding rock, causing the angle of the blasting stress wave incident on the free face of the roadway surrounding rock to be different and resulting in differences in the dynamic response of the roadway surrounding rock. With the decrease in the distance from the blasting source to the roadway surrounding rock, the difference in particle velocities of the surrounding rock on each side was more pronounced.
It is shown that the relative angle (θ) significantly influences the dynamic response and stress distribution in the surrounding rock on each side. The numerical results are consistent with the theoretical results. Therefore, considering θ as a major factor that affects the vibration of surrounding rock in open-pit blasting is imperative.