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A THREE DIMENSIONAL FINITE VOLUME MODEL FOR ACID MINE DRAINAGE SIMULATION IN OPENCAST MINE BACKFILL

机译:Opencast矿井回填中酸性矿井排水仿真三维有限体积模型

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The backfill of opencast mines often contains pyrite which may be oxidised and produce acid mine drainage (AMD) if it is exposed to the atmosphere. AMD is often characterised by high concentrations of iron, high sulphate and low pH and it is Considered to be a major cause of long-term poor water quality and is the source of many environmental problems. This paper presents a three dimensional numerical model that incorporates oxygen balance, pyrite oxidation, groundwater flow and transport of the oxidation products in order to describe the long-term pyrite oxidation and pollutant leaching within the backfill of an opencast mine. A diffusion process governs the oxygen transport within the pore space of the backfill. A shrinking-core concept describes the oxidation of pyrite particles. The transport model incorporates physical processes (advection, diffusion) and chemical processes. A multi-purpose CFD (computational fluid dynamics) software called PHOENICS version 3.6.1 incorporating a numerical finite volume discretisation scheme has been modified by creating a PHOENICS pre-processing input file in the PHOENICS input language (Q1_AMD_3D) and developing a subroutine called GROUND_ AMD3D in the FORTRAN 99 language. One and two dimensional modelling was performed to calibrate the three dimensional model. It was found that the oxidation of only a small fraction of pyrite is enough to cause long-term environmental problem due to acid mine drainage generation. The lowering of pH in the range between 2.5 to 3.5 results in the bacterial oxidation of pyrite being enhanced. Subsequently the bacterial action produces more Fe~(3+), SO_4~(2-) , H~+ and Fe~(2+) . The results obtained from three-dimensional modelling can be used for designing an effective site remediation program in order to minimise environmental effects arising from abandoned backfilled opencast mines.
机译:露天矿的回填常常含有黄铁矿如果暴露于大气中,其可被氧化并产生酸矿山排水(AMD)。 AMD的特点往往是高浓度的铁,硫酸盐高和低pH值的,它被认为是长期的水质差的一个主要原因,是许多环境问题的根源。本文提出了一种三维数字模型并入氧平衡,黄铁矿氧化,地下水流和氧化产物的运输,以便描述露天矿的回填内长期黄铁矿氧化和污染物浸出。扩散过程支配的回填孔隙空间内的氧运输。甲收缩芯概念描述黄铁矿颗粒的氧化。传输模型包括物理过程(平流,扩散)和化学过程。一种多用途称为PHOENICS版本3.6.1掺入数值有限体积离散方案CFD(计算流体动力学)软件已经通过创建PHOENICS改性前处理在PHOENICS输入语言(Q1_AMD_3D)输入文件和显影被叫GROUND_子程序AMD3D在FORTRAN语言99。进行一个维和二维模型校准三维模型。结果发现,只有黄铁矿的一小部分的氧化是足以引起长期的环境问题,由于酸性矿井水的产生。 pH值在2.5至3.5的结果在黄铁矿的细菌氧化之间的范围内的降低而提高。随后将细菌作用产生更多的Fe〜(3+),SO_4〜(2-),H〜+和Fe〜(2+)。从三维模型得到的结果可以用于以减少废弃回填露天矿产生的环境影响的设计有效的现场整治方案。

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