吸附
氢氧化物
锌
浸出(土壤学)
氢氧化锌
锗
胶体
化学
无机化学
氧化物
化学工程
材料科学
硅
有机化学
土壤水分
土壤科学
工程类
环境科学
作者
Ming Liang,Yan Hong,Haokai Di,Kun Yang,Libo Zhang
出处
期刊:Langmuir
[American Chemical Society]
日期:2024-06-11
卷期号:40 (25): 13167-13176
被引量:7
标识
DOI:10.1021/acs.langmuir.4c01167
摘要
In the leaching process of secondary zinc oxide, there is a problem of germanium loss caused by the colloidal adsorption of germanium by iron hydroxide (Fe(OH) 3 ) formed by Fe 3+ hydrolysis. In response to this, this article elucidates the hydrolysis conditions of Fe 3+ and the adsorption mechanism of the Fe(OH) 3 colloid on germanium through theoretical analysis and simulation of the adsorption process. The coexistence of Fe 3+ and H 2 GeO 3 requires high acidity conditions (pH < 1.53 at 25 °C). The adsorption of germanium by the Fe(OH) 3 colloid is a spontaneous exothermic entropy reduction process, which conforms to a pseudo-second-order kinetic model and includes three stages: fast, slow, and equilibrium. In addition, the adsorption process can be fitted by the Langmuir isotherm adsorption model, mainly consisting of monolayer and chemical adsorption. The Fe(OH) 3 colloid has a great adsorption capacity for germanium at 328 K, and the equilibrium adsorption capacity is 261.15 mg/g in 40 min. During leaching, the adsorption of germanium by Fe(OH) 3 colloids can be inhibited by increasing the reaction temperature, controlling the pH value of the solution system, and suppressing the formation of Fe 3+ at the source. This study provides direction for how to suppress the adsorption of germanium by Fe(OH) 3 colloids during the leaching process of secondary zinc oxide, which is of great significance for improving the germanium leaching efficiency and fully utilizing limited germanium resources.
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