Abstract

In underground mines, excavating disturb the initial equilibrium state of the rock mass, and therefore require selection of a support in order to control the movement of rocks, avoid landslide and work safely. Thus, the progress of mining operations in the ST2 mineralization, in the eastern zone of the Bouazzer mine, is disrupted because of stability problems. On the basis of field observations and analyzes of core drill, the geological and structural study, carried out in this area, has shown the existence of three types of facies: altered and cracked diorite, cobaltiferous mineralization which is in contact with serpentinites. In fact, the empirical methods such as Barton, Bieniawski and the recommendations of the AFTES have qualified the rock mass as poor, furthermore they proposed as kind of supports: steel arches, shotcrete and rock-bolts. Numerical simulation by the finite element method proved to be very complex due to existence of several types of discontinuities (faults, shistosities and joints).These discontinuities are natural fractures that delimit various shapes and sizes of wedges, which can become detached from the roof or siding of the excavation and collapse under their own weight. Although the empirical methods cited above provide supports for each facies, however, this support is expensive and difficult to implement in practice because it must cover the entire surface of the excavation and thus not allowing to detect stable blocks that do not require a support. For this it was essential to carry out an analysis of wedges to better locate unstable blocks. The treatment of fracturing data has highlighted the presence of five sets of discontinuities of which three sets are principals and the other two are minor joints. Then, while taking into account the geometrical, mechanical data of the discontinuities as well as the geometrical data of the excavation, we were able to detect the shape and the size of the unstable blocks and the sets of discontinuities delimiting them and which favor their sliding and tilting. Thus, we calculated the number of anchor bolts needed to stabilize these blocks in order to ensure an acceptable safety factor. This study shows clearly how a wedge analysis of the rock mass can guide and optimize the support work.

Highlights

  • To exploit the depth-seated mineralization of cobalt at Bou-Azzer mine, underground excavations are executed

  • The tunnel orientation, orientation and properties of main joint sets, and rock properties as well as the state of stress in the field are introduced in Unwedge, After this, we could detect and visualize the key blocks on Unwedge, Once they are located, we check the value of the safety factor if it is satisfy the condition (Fs> 1.5), if yes we will not need a support as the blocks ensure their own stability thanks to the friction between them joints

  • - For the quartz diorites : For the quartz diorites, we first studied stability of wedges located in the periphery of a rectangular excavation (2.5*2.5) in the serpentinite, and we found that the upper right and roof wedges are instable since the safety factor is less than 1.5

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Summary

Introduction

To exploit the depth-seated mineralization of cobalt at Bou-Azzer mine, underground excavations are executed. The mineralization exploited is in the form of vein, with a subvertical dip and variable thickness, collected between the serpentines and the quartz diorites of the Precambrian II Inferior. The progress of the mining operations is often disturbed because of stability problems of the rock mass, that may harm safety of mine workers, materials, and negatively impacts the production in the working sites. We will firstly present the characterization results of a rock mass by empirical methods (Deere, Barton, Beniawski, Aftes, Hoek and Brown) and the modes of support recommended ensuring the stability of the rock mass. By using the Unwedge program, based on Goodman-Shi key block theory [3], we will study the instable blocks and design an appropriate and optimized support for these blocks.

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