Research Article  Open Access
Nan Jiang, Chuanbo Zhou, Xuedong Luo, Shiwei Lu, "Damage Characteristics of Surrounding Rock Subjected to VCR Mining Blasting Shock", Shock and Vibration, vol. 2015, Article ID 373021, 8 pages, 2015. https://doi.org/10.1155/2015/373021
Damage Characteristics of Surrounding Rock Subjected to VCR Mining Blasting Shock
Abstract
For limiting the damage range caused by explosive shock loads in vertical crater retreat (VCR) mining, the blasting damage characteristics of surrounding rock were studied by two methods: numerical simulation and ultrasonic testing. Combined with the mining blasting in Dongguashan Copper Mine of China, the VCR blasting shock characteristics under different conditions are obtained by using LSDYNA. Based on statistical fracture mechanics and damage mechanics theories, a damage constitutive model for rock mass subjected to blasting shock load was established. Then by using the fast Lagrange analysis codes (FLAC3D), the blasting damage characteristics of surrounding rock were analyzed by applying the blasting shock loads obtained from the VCR mining and the damage zone is obtained. At last, the relationship between the amount of explosives and the radius of damaged surrounding rock mass was discussed, and its formula was also derived. The research provides a theoretical basis for rationally controlling stope boundaries and optimizing mining blasting parameters.
1. Introduction
VCR (vertical crater retreat) mining technology is widely used in mine engineering because it possesses many better features, such as higher efficiency and more simple operation. In the mining process, the blasting shock originating simultaneously from the rockfracturing blasting load also can damage surrounding rock. For better control of the stope boundary, it is a key prospect in engineering application to ascertain damage characteristics of surrounding rock under mining blasting shock load and to optimize blasting parameters.
Damage effects of rock mass under blasting load were extensively studied at home and abroad, but these researches were mostly based on insite tests and laboratory experiments [1–4]. In recent years, with the development of computer technology, numerical simulation was increasingly adopted to study blasting damage of rock mass [5–8]. Hao et al. analyzed the rock damage under stress wave of blasting based on an anisotropic damage constitutive model [9, 10]. Wei et al. studied the damage of rock mass subjected to underground explosion [11]. Wang et al. analyzed the tensile damage of brittle rock mass subjected to underground explosion and the evolution characteristics of craters [12].
Based on the theories in statistical fracture mechanics and damage mechanics, a damage model for rock mass subjected to blasting load was established. At the same time, damage characteristics of surrounding rock subjected to mining blasting shock load in VCR mining and conventional blasting shock load were analyzed by numerical simulations.
2. VCR Mining Blasting Shock Load
2.1. Numerical Model
Dongguashan Copper Mine is located in Tongling, Anhui, China. It has the ability to produce around 4.3 million tons of copper ore annually, and its service life is 28 years. As the largest copper mine of downhole pit mining in Asia, its mining depth is more than 1000 meters, which ranks the first among the nonferrous metal mines in Asia. The deposit is as long as more than 1800 m in trend, more than 500 meters wide, and 20–70 m thick. It is divided into panels every 100 m, and there is an 18 m wide barrier pillar in each pair of adjacent panels. A panel is 100 m wide, whose length and height equal the width and the thickness of the deposit, respectively. Every panel consists of 20 stopes, which are arranged along the trend of the deposit and 18 m wide. The room stope and pillar stope are 82 m long and 78 m long, respectively. In the mining blasting process, it is significant to control the stope boundary for safety of underground mining construction in the mine.
VCR mining method was adopted for underground mining in Dongguashan Copper Mine. According to the reality, largediameter deephole blasting is introduced. The blasthole diameter is 165 mm, the charge length is 1.5 m to 10.5 m, and the stemming length is 1.2 m to 2.0 m. In this study, a threedimensional model is established using the software LSDYNA, as shown in Figure 1, which is measuring 20 m in direction, 20 m in direction, and 10 m in direction. 10 blasting holes are equally divided into 2 rows. The distance between two rows is 3 m, and the distance between 2 adjacent holes in the same row is 2.8 m. Only the bottom surface is free, and the remaining surfaces are applied with nonreflecting boundary.
2.2. Calculation Parameters
In LSDYNA simulation, MohrCoulomb (MC) model is selected as rock material’s model [13]. According to the test results, parameters of stope rock mass are listed in Table 1.

The JWL state equation can simulate the relationship between pressure and specific volume in the explosion process [14]. The equation is as follows:where , , , , and are material constants, is pressure, is relative volume, and is specific internal energy. The physical and mechanical parameters of the dynamite are the same as those of the field test and are listed in Table 2.

2.3. Blasting Load
Due to the model which is built symmetrically, a quarter of the model is calculated to reduce the size of the research object. So the model was simplified as a 10 m cube, and the charge length is 3 m, 3.5 m, 4.0 m, 4.5 m, 5.0 m, 5.5 m, and 6.0 m, respectively. The charging length of 6.0 m is shown in Figure 2. The bottom surface is free; the front surface and the right surface are applied with normal displacement constraint. The remaining surfaces are applied with nonreflecting boundary, and the left sides are stope boundaries [15].
As illustrated in the rock blasting theory, the crushed zone radius is 23 times larger than the blasthole radius [16]. In order to obtain the blasting load applied on the crushed zone boundary, the monitoring element was selected at a horizontal distance of 0.33–0.50 m away from the center of the blasthole. For example, when the charge length is 6 m, Element H54050 was selected as the monitoring element, as shown in Figure 3.
Figure 4 shows the pressure curve with time at Element H54050. Shock wave pressure applied on the boundary of crushed zone under blasting load increases to its maximum within 0.5 ms, up to 1.74 GPa. In the same way, when the charge length is 3 m, 3.5 m, 4 m, 4.5 m, 5 m, and 5.5 m, the maximum shock wave pressure applied on the boundary of crushed zone under blasting load is 1.4 GPa, 1.43 GPa, 1.46 GPa, 1.52 GPa, 1.57 GPa, and 1.61 GPa, respectively.
3. Rock Damage Model under Blasting Shock Load
According to statistical fractured mechanics [17], rock damage is believed to occur when the crack density reaches a given value, and the cumulation and growth of crack in rock can be demonstrated in probability terms. The following agreements have been achieved by the related research [18, 19]:(1)a rock material does not fail if the applied stress is lower than its static strength;(2)when a rock material is subjected to a stress higher than its static strength, a certain time duration is needed so that the fracture can take place;(3)the dynamic fracture stress of a rock material is higher than its static strength and is approximately cube root dependent on the strain rate.
So damage due to blasting loading can be defined as the probability of fracture, written as follows:where is the fail probability of damaged rock mass, is the crack density in direction, and is damage value. Obviously has a value between 0 and 1, to respond to the stiffness of the intact, undamaged rock with crack density , and the fully fragmented rock with an infinite , respectively. Crack density is defined as follows:where , are material constants, is the principle strain in direction, is the corresponding critical strain, and is the time to reach fracture stress. In terms of isotropic damage, the principle strain would be equivalent volume modulus.
Tensile strain is a quite important index to evaluate whether rock mass is damaged or not [20], so generally uniaxial tensile test is adopted to approximately simulate rock damage. Critical strain can be obtained based on uniaxial tensile test as follows:where is static tensile strength in direction and is equivalent elastic modulus. We define and as the tensile strain and crack density in direction when rock mass is cracked. Then can be expressed as follows:where is the total time when the rock mas reaches the fracture stress and is the time duration when the tensile strain reaches the critical value. Both of them can be obtained bywhere is tensile strain rate. Accordingly, (5) can further be written asThe time interval between the critical damage to the fracture of rock mass is given byThe relationship between the fracture stress and the corresponding strain isSubmitting (4) and (8) to (9), the strain rate dependent constitutive relation is obtained:where is the damage variable under the fracture state and other variables are the same as previous meanings. Because the dynamic tensile strength of a rock material is higher than its static strength and is approximately cube root dependent on the strain rate, the value of can be given as 2. For given and , the material constant can be calculated based on the blasting crater test results.
According to the Construction Technical Specification on RockFoundation Excavation Engineering of Hydraulic Structure (SL4794), should be 0.2 [21]. At the same time, based on the insite tests, is equal to 3.16 × 10^{6}, and other parameters are listed in Table 1.
4. Numerical Analysis of Rock Damage Zone
4.1. Numerical Model
Like the blast model above, a 3D model was established using FLAC3D. Hexahedral solid element is selected when the model is meshed. Due to the model which is built symmetrically, a quarter of the model is calculated to reduce the size of the research object. For example, when the charge length is 6 m, a 10 m long, 14 m wide, and 14 m high model is established, as shown in Figure 5. The left side is the stope boundary, and the hollow part is the boundary of crushed zone of 2 m × 6 m × 7.5 m.
The boundary conditions are the same as those in Section 2.3. because the maximum pressure varies depending on the charge and the blasting damage zone depending on the charge can be simulated by applying different pressure on the boundary of crushed zone. MohrCoulomb (MC) model is considered the material model for numerical simulation [22], and the parameters are listed in Table 1. The applied dynamic loads are equal to the results calculated above.
4.2. Analysis of the Damage Characteristics
For example, when the charge length is 6 m, the damage growth on the free surface and along the height direction is shown in Figures 6 and 7.
Figures 6 and 7 show that the rock mass is not damaged yet in 0.1 ms after detonation whether on the free surface or along the height direction. The damage of rock subject to blasting load needs some time to develop. In the time interval between 0.1 ms and 1.5 ms, the damage zone radius is approximately 6.785 m and it reaches about 8.142 m in the time interval between 1.5 ms and 3.0 ms. Combined with the above analysis, the calculation results agree well with the first two agreements and which are presented in Section 3.
Using the same way, the damage zone with the charge length of 3 m, 3.5 m, 4.0 m, 4.5 m, 5.0 m, 5.5 m, and 6.0 m is shown in Figure 8. Damage under blasting loads grows faster within the first 1.5 ms after denotation than that in the latter 1.5 ms.
Figure 8 shows the crushed zone with the damage value of 0.2. The damage zone radiuses are listed in Table 3.

Based on the insite parameters, the statistical relationship between charge amount and damage zone radius is established.
As shown in Figure 9, the function relation can be expressed bywhere is damage zone radius of surrounding rock and is onestage charge.
The rooms and barrier pillars are 18 m wide. As illustrated in (11), when m, the maximum onestage charge is 1848.26 kg. So the insite maximum onestage charge should be less than 1848.26 kg. The maximum onestage charge can be precalculated by empirical formula when the blasting operation is performed at any location in the stope, so that the stope boundary can be under control, the surrounding rock mass can be stable, and the safe production can be ensured.
5. Conclusions
The following conclusions can be drawn. (1)Based on statistical fracture mechanics, damage due to blasting shock load can be defined in the probability form. The damage model was established. And the damage characteristics were obtained by numerical simulation.(2)Under blasting shock load, the rock mass is not damaged yet at the initial stage after detonation whether on the free surface or along the height direction. The damage of rock subject to blasting load needs some time to develop. Damage under blasting loads grows faster within the first 1.5 ms after denotation than that in the latter 1.5 ms.(3)According to the results in different blasting conditions, the statistical relationship between charge amount and damage zone radius is established. Furthermore, the maximum onestage charge was proposed to be less than 1848.26 kg on the purpose of controlling the stope damage boundary.
Conflict of Interests
The authors declare that there is no conflict of interests regarding the publication of this paper.
Acknowledgments
The study was sponsored by the National Natural Science Foundation of China (Grant nos. 41372312 and 51379194), the Fundamental Research Funds for the Central Universities, China, University of Geosciences (Wuhan) (Grant no. CUGL140817), and the China Postdoctoral Science Foundation (Grant no. 2014M552113). The authors are also grateful to the China Scholarship Council (CSC) for the support.
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Copyright
Copyright © 2015 Nan Jiang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.