Molson J W, Fala O, Aubertin M, Bussière B
Department of Civil, Geological and Mining Engineering, Ecole Polytechnique de Montréal, P.O. Box 6079, Stn. Centre-ville, Montréal, Québec, Canada H3C 3A7.
J Contam Hydrol. 2005 Aug;78(4):343-71. doi: 10.1016/j.jconhyd.2005.06.005.
Numerical simulations of layered, sulphide-bearing unsaturated waste rock piles are presented to illustrate the effect of coupled processes on the generation of acid mine drainage (AMD). The conceptual 2D systems were simulated using the HYDRUS model for flow and the POLYMIN model for reactive transport. The simulations generated low-pH AMD which was buffered by sequential mineral dissolution and precipitation. Sulphide oxidation rates throughout the pile varied by about two orders of magnitude (0.004-0.4 kg m-3 year-1) due to small changes in moisture content and grain size. In the fine-grained layers, the high reactive surface area induced high oxidation rates, even though capillary forces kept the local moisture content relatively high. In waste rock piles with horizontal layers, most of the acidity discharged through vertical preferential flow channels while with inclined fine grained layers, capillary diversion channeled the AMD to the outer slope boundary, keeping the pile interior relatively dry. The simulation approach will be useful for helping evaluate design strategies for controlling AMD from waste rock.
本文给出了含硫化物的层状非饱和废石堆的数值模拟结果,以说明耦合过程对酸性矿山排水(AMD)产生的影响。利用HYDRUS模型进行水流模拟,POLYMIN模型进行反应输运模拟,对概念性二维系统进行了模拟。模拟产生了低pH值的AMD,其通过矿物的顺序溶解和沉淀得到缓冲。由于含水量和粒度的微小变化,整个矿堆中的硫化物氧化速率变化约两个数量级(0.004 - 0.4 kg m-3年-1)。在细颗粒层中,尽管毛细力使局部含水量相对较高,但高反应表面积导致了高氧化速率。在具有水平层的废石堆中,大部分酸性物质通过垂直优先流通道排出,而在具有倾斜细颗粒层的废石堆中,毛细导流将AMD引导至外坡边界,使矿堆内部相对干燥。该模拟方法将有助于评估控制废石产生AMD的设计策略。