基于直接作用、间接作用、复合作用3种传统微生物浸矿机制,结合堆浸体系内细菌种类(吸附细菌、游离细菌)、废石结构、Fe3+迁移特征,提出直接间接作用和间接接触间接作用微生物浸蚀机制,探讨浸出过程废石力学损伤机理;将溶液对废石的生化侵蚀划分为溶蚀、沉淀胶结、结晶膨胀3个阶段,分析不同阶段废石力学性质的变化趋势。研究结果表明:废石在酸性溶液中浸泡45 d后的破裂裂纹比未浸泡、浸泡15 d、浸泡30 d的废石要复杂、曲折;浸泡45 d后,废石黏聚力降低87.7%,废石破坏时的剪应力和正应力均降低一半;浸泡后废石表面铜矿物等物质被溶解,表面微裂隙及孔洞得到进一步发育和扩展。
Interaction between bacteria and rock was divided into three traditional mechanisms, i.e direct, indirect and combined bioleaching. Two new mechanisms, i.e direct-indirect and indirect-contact indirect bioleaching were put forward by analysizing the bacterium category (attached and non-attached), rock inner structure and transportation of Fe3+ Damnification of the rock mechanical properties during bioleaching was investigated. The evolution of the mechanical properties in different stages was analyzed. Experiment was conducted to investigate the mechanical properties of the attacked rock. The results show that dissolution, cementation of precipitation and crystal swell are the main stages during the leaching process, breaking cracks of the rock immersed by acid solution for 45 d are more complicated and twisted than the unattacked rock and attacked for 15 d and 30 d. Moreover, the rock cohesion decreases by 87.7% after being attacked for 45 d, and both normal and shear strength of the rock decreases by 50%. The copper minerals are dissolved by the acid solution, and fractures and cracks of the leached rock are developed deeply.