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Inter-particle liquid spread pertaining to heap leaching using UV fluorescence based image analysis

机译:使用UV荧光的图像分析与堆浸出有关的颗粒液体涂抹

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The visualisation of individual flow paths in a porous media and how they relate to the overall hydrodynamics is crucial to improving our understanding of a number of systems. Unsaturated flow through larger particles (order of millimetres and a few centimetres) in heap leaching systems where both gravity and capillarity play an important role in the structure of the flow paths is complex and still not fully understood. A variety of laboratory methods have been employed for this purpose, with UV light being used in several studies. Flow studies have typically involved millimetre and sub-millimetre scale particles and the flow is typically capillary-dominated. This paper instead concentrates on gravity-dominated flows pertaining to heap leaching and is particularly focused on developing methods for using the UV fluorescence to obtain quantitative measurements of liquid spreading, such as average lateral liquid spread for a point source liquid addition. This study uses a pseudo2-D system with larger ore particles than in previous UV flow studies. The UV fluorescence results were analysed using image analysis to determine the overall liquid spreading and the locations of the flow paths. Both narrowly sized and realistic ore systems were investigated to understand the effect of length scale on flow paths and dynamics of liquid spreading through the gravity-dominated ore beds. It was shown that both ore systems experience distinct flow channelling compared to the more uniform flow profiles observed in capillary-dominated systems. Lateral liquid spreading coefficients were calculated, with the narrowly sized ore system showing higher values, probably due to the larger effective length scale of the inter-particle spaces.
机译:多孔介质中的个体流动路径的可视化以及它们与整体流体动力学的关系是至关重要的,从而提高我们对许多系统的理解。在堆浸出系统中,通过较大的颗粒(毫米和几厘米)的不饱和流动,其中重力和毛细血管性在流动路径的结构中发挥着重要作用,仍然没有完全理解。为此目的采用了各种实验室方法,在几项研究中使用UV光。流动研究通常涉及毫米和亚毫米级颗粒,并且流动通常是毛细管主导的。本文集中在与堆浸出有关的重力主导流体,特别关注使用UV荧光的方法以获得液体扩散的定量测量,例如用于点源液的平均横向液体。该研究使用具有较大矿石颗粒的假型2-D系统而不是先前的UV流程研究。利用图像分析分析UV荧光结果以确定整个液体扩散和流动路径的位置。研究了狭义和现实的矿石系统,以了解长度尺度对通过重力占据矿床的流动路径和液体涂抹的动力学的影响。结果表明,与毛细管主导系统中观察到的更均匀的流动曲线相比,两个矿石系统经历了不同的流动窜流。计算横向液体扩展系数,具有狭窄的矿石系统,显示出更高的值,可能是由于颗粒间空间的较大的有效长度尺度。

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