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Dynamic behavior of flow during leaching of copper ores

机译:铜矿浸出过程中流动的动态行为

摘要

The objective of this investigation was to experimentally determine the variation in the flow characteristics of tactite copper ores during the leaching process. The laboratory work involved estimation of porosity and permeability of cores before leaching, and after various intervals of leaching. The tests were carried out using specimens of diameter 1.5 and 4.0 inches, prepared from boulders obtained from the Cyprus Casa Grande mine. A solution containing about 25 grams of sulfuric acid per liter was used as the lixiviant. Porosity was determined using the water saturation method. The permeability was estimated using either helium or water with the specimens stressed triaxially to simulate in situ conditions. The rate of copper recovery from the specimen during the leaching process was also determined by estimating the copper content in the solution used for leaching. The results indicate that the permeability and porosity of the specimens increased with leaching, but both tend to remain constant after most of the soluble material in the core was dissolved. The rate of copper recovery was high initially but dropped as leaching progressed and the copper in the specimen was depleted.
机译:这项研究的目的是通过实验确定针状铜矿在浸出过程中的流动特性变化。实验室工作涉及在浸出之前和不同浸出间隔之后估算岩心的孔隙率和渗透率。使用从塞浦路斯卡萨格兰德矿获得的巨石制备的直径为1.5和4.0英寸的样品进行测试。每升含约25克硫酸的溶液用作浸滤剂。孔隙率使用水饱和法测定。使用氦气或水估计渗透率,并通过三轴应力模拟现场条件。浸出过程中样品中铜的回收率也通过估算浸出溶液中的铜含量来确定。结果表明,样品的渗透率和孔隙率随浸出而增加,但在岩心中的大多数可溶物质溶解后,两者往往保持恒定。铜的回收率最初很高,但随着浸出的进行而下降,并且样品中的铜耗尽。

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