单孔爆破中炸药和岩石质量特性对爆破损伤的影响

Mining Pub Date : 2024-03-20 DOI:10.3390/mining4010011
Magreth S. Dotto, Y. Pourrahimian
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引用次数: 0

摘要

在采矿生产的岩石爆破中,应力波和爆炸气体在岩石破碎中起着重要作用。更好的能量分布可改善破碎效果和安全性,降低生产成本,提高生产率,控制矿石损失和稀释。爆破效果因炸药的选择和所遇岩体的性质而有很大不同。本研究利用案例研究的数据,通过数值模拟分析了岩体和炸药特性对爆破结果的影响,随后通过现场爆破破碎验证了模拟结果。研究结果表明,对于一组给定的岩石属性,炸药的选择对破碎结果有重大影响。烈性炸药(高 VOD 和爆炸压力)有利于在坚硬的岩石中形成大的断裂范围,而弱性炸药则能更好地分布爆炸能量和断裂。岩石结构(如岩石接触点和节理)的存在会影响应力波和断裂的传播,这取决于结构的材料特性、强度和方向,以及应力波的方向和强度。当应力波遇到接触点时,根据其方向,应力波从软到硬会增强,反之则会减弱。应力波在接触面反面造成断裂的能力取决于透射波的强度和岩石的强度。透射波强度是入射波强度和界面材料之间阻抗差的函数。岩体中节理的存在会影响应力波的传播,主要取决于填充材料的特性和应力波接近节理的角度。可压缩性较低、刚度较高的节理会传递更多的能量。在应力波垂直冲击接缝的区域也会传递更多的能量。与自由面平行的接缝会在接缝的另一侧产生额外的断裂。其他参数,如接缝宽度、连续性、断裂频率以及与装药的距离,都会增强效果。为了实现有效的破碎,爆破设计应通过炸药选择和模式设计来减轻岩体变化的影响,以确保在几何设计的限制范围内实现足够的能量分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Influence of Explosive and Rock Mass Properties on Blast Damage in a Single-Hole Blasting
In rock blasting for mining production, stress waves play a major role in rock fracturing, along with explosive gases. Better energy distribution improves fragmentation and safety, lowers production costs, increases productivity, and controls ore losses and dilution. Blast outcomes vary significantly depending on the choice of the explosive and the properties of the rock mass encountered. This study analyzes the effects of rock mass and explosive properties on blast outcomes via numerical simulation using data from the case study, and later validates the simulation results from the field blast fragmentation. The findings suggest that, for a given set of rock properties, the choice of explosive has a major influence on the resulting fragmentation. Strong explosives (high VOD and detonation pressure) favor large fracture extents in hard rocks, while weaker explosives offer a better distribution of explosive energy and fractures. The presence of rock structures such as rock contacts and joints influences the propagation of stress waves and fractures depending on the structures’ material properties, the intensity and orientations, and the direction and strength of the stress wave. When the stress wave encounters a contact depending on its direction, it is enhanced when traveling from soft to hard and attenuates in the opposite direction. The ability of the stress wave to cause fracturing on the opposite side of the contact depends on the intensity of the transmitted wave and the strength of the rock. Transmitted wave intensity is a function of the strength of the incident wave and the impedance difference between the interface materials. The presence of joints in the rock mass affects the propagation of the stress wave, mainly depending on the infill material properties and the angle at which the stress wave approaches the joint. Less compressible, higher stiffness joints transmit more energy. More energy is also transmitted in the areas where the stress wave hits the joint perpendicularly. Joints parallel to the free face offer additional fracturing on the opposite side of the joint. Other parameters, such as the joint width, continuity, fracture frequency, and the distance from the charge, enhance the effects. To achieve effective fragmentation, the blast design should mitigate the effect of variability in the rock mass via explosive selection and pattern design to ensure adequate energy distribution within the limits of geometric design.
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