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A model of long-term oxidation and leaching processes in pyritic coal cleaning wastes

机译:黄铁矿清洁废物中长期氧化和浸出过程的模型

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This study presents a numerical model to simulate a long-term pyrite oxidation process and subsequent multi-component reactive transportation of the oxidation productions in an abandoned coal waste pile in Northeast of Iran. For this purpose, 240 solid samples of wastes were obtained from different depths of 10 vertical trenches excavated in the pile. Then, geochemical analyses, including determination of pyrite content remaining in the waste particles, paste pH tests, sulfate concentration, were conducted on the collected samples. In addition, oxygen concentration profile associated with each trench was determined. The results show that the oxidation zone is limited to the shallower depths of the pile where oxygen was readily available. Furthermore, governing mathematical equations describing oxygen transport, pyrite oxidation, and transport of oxidation products were formulated based on the fact that the oxidation process follows a shrinking core concept, and gaseous diffusion is the main process for oxygen supply within the waste materials. The transport equation incorporates physical processes of advection and dispersion. Eventually, an existing one-dimensional numerical finite volume model was slightly modified, and the governing equations were simultaneously solved using a commercial computational fluid dynamics software called PHOENICS by providing extra codes for those terms of equations which are not included in PHOENICS governing equation. The results of simulation for 15 years of abandoned of the pile showed close agreement with the geochemical data. The simulations were further performed to predict the pyrite oxidation and subsequent transportation processes for years 5, 10, and 20 from now. The results revealed that more load of the oxidation products would be expected than those are generated now, and the products would reach the pile base. It will result in environmental problems for soil, surface, and groundwater of the study area and nearby lands in future.
机译:这项研究提供了一个数值模型,用于模拟伊朗东北部废弃煤waste石中长期黄铁矿氧化过程以及随后的氧化产物多组分反应性运输。为此,从堆中挖掘的10个垂直沟槽的不同深度获得了240个固体废物样品。然后,对收集的样品进行了地球化学分析,包括确定废物颗粒中残留的黄铁矿含量,糊状pH测试,硫酸盐浓度。另外,确定与每个沟槽相关的氧浓度分布。结果表明,氧化区仅限于较易获得氧气的较浅深度。此外,基于氧化过程遵循收缩核概念,而气体扩散是废物中氧气供应的主要过程,从而制定了描述氧气输送,黄铁矿氧化和氧化产物输送的主导数学方程式。输运方程式包含对流和扩散的物理过程。最终,对现有的一维数值有限体积模型进行了轻微修改,并使用称为PHOENICS的商业计算流体动力学软件,通过为PHOENICS控制方程未包含的那些方程项提供了额外的代码,同时求解了控制方程。 15年弃置桩的模拟结果与地球化学数据非常吻合。从现在开始,进一步进行了模拟以预测黄铁矿的氧化和随后5年,10年和20年的运输过程。结果表明,预计氧化产物的负载量将比现在产生的负载更多,并且氧化产物将到达桩基。将来会导致研究区域和附近土地的土壤,地表和地下水的环境问题。

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