Simulation of coupled flowing-reaction-deformation with mass transfer in heap leaching processes

Governing equations for a fully coupled flowing-reaction-deformation behavior with mass transfer in heap leaching are developed. The model equations are solved using an explicit finite difference method under the conditions of invariable application rate and constant hydraulic head. The distribution of the degree of the saturation, as well as the distributions of the concentration of the reagent and the solute is given. A cubic relationship between the mineral recovery and the leaching duration is obtained based on the numerical results. The relationship can be used to predict the recovery percentage of the valuable metal.     

水口山铅锌矿4#金矿体矿石室内试验

对水口山铅锌矿4~#金矿体矿石进行了氰化物和硫脲室内浸出可行性研究,初步试验结果表明,可行性方案为氰化浸出工艺,并研究了氰化浸出工艺浸出剂浓度、氧化剂浓度、液固比等对浸出效果影响,金浸出率超过90％,获得了浸出的合适参数和工艺条件,可为下步现场试验提供参考依据。     

碳酸盐岩溶蚀作用中Cd的淋溶/残余行为

揭示碳酸盐岩溶蚀作用中镉(Cd)的淋溶/残余行为是完整理解碳酸盐岩风化剖面形成与演化过程中Cd的地球化学的重要环节。本文对一件白云岩试样进行了淋溶实验,设计了收集淋溶残余物与淋出液的两种装置,随淋溶进程,对淋溶残余物及淋出液相关组分进行了测试。贫Cd碳酸盐岩中的Cd(0.12 mg/kg)在酸不溶相富集(0.98 mg/kg),且样品中酸不溶物质量分数仅为2.48%。由于酸不溶物质量分数极低,酸溶相中Cd占全岩中Cd的质量比仍具有绝对优势。碳酸盐岩溶蚀过程中,在排水条件良好的条件下,酸溶相的Cd随碳酸盐溶解而淋失,酸不溶相的Cd随酸不溶物在淋溶残余物中的集聚而富集。碳酸盐岩溶蚀形成残积土的过程就是基岩中大量Cd绝对淋失与少量Cd显著相对残余富集的过程。