“钙化-钾碱”体系下高岭石水浸法制备硅酸铝钾矿物硅钾肥的研究

IF 5.3 2区 地球科学 Q2 CHEMISTRY, PHYSICAL
Qingdong Li , Guozhi Lv , Shuojia Song , Renyun Zhang , Xin He , Fangyi Yuan , Zhuangzhuang Yun , Tingan Zhang
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引用次数: 0

摘要

高岭石是铝土矿中常见的典型硅酸盐矿物,在拜耳法中易与水合硅酸铝钠(赤泥)结合为平衡固相。这种组合导致氧化铝和碱的损失增加,造成环境污染。高岭石和其他铝和硅矿物相被认为是氧化铝生产中的有害杂质。它们的去除使处理过程复杂化,增加了生产成本,并且不能从根本上解决赤泥的积累和排放问题。本研究提出了“钙化-钾碱”(CPA)工艺,以钾肥代替钠碱,模拟拜耳法中铝土矿含硅原生矿相高岭石的水热浸出过程。转化产物为嗜钾石(KAlSiO4),可用于制备矿物基硅钾肥。研究了高岭石在浸出过程中的溶解行为及机理。浸出实验和分析(FTIR、XRD、XRF、XPS和SEM-EDS)表明,氧化钾浓度和碱浸温度是影响高岭石转化的主要因素。最佳溶解条件为温度200℃、钙硅比0.2、K2O浓度160 g/L、反应时间60 min。在此条件下,高岭石的反应率可达98.9%,产硅酸铝钾。此外,重金属含量等指标达到相关标准,可将其掺入有机质中,制备无机硅钾肥,部分替代农业上的工业肥料,具有显著的成本优势,市场前景广阔。该工艺将废铝土矿中的含硅矿物相转化为有价值的资源,为中低品位铝土矿的利用和赤泥的处理提供了新的参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on the preparation of mineral silicon-potassium fertilizer by hydrothermal leaching of kaolinite to generate potassium aluminosilicate under the “calcification-potash alkali” system
Kaolinite is a typical silicate mineral found in bauxite, which tends to combine with sodium aluminosilicate hydrate (red mud) as the equilibrium solid phase in the Bayer process. This combination leads to increased losses of alumina and alkali, resulting in environmental pollution. Kaolinite and other aluminum and silica mineral phases are considered harmful impurities in alumina production. Their removal complicates the treatment process, increases production costs, and does not fundamentally address the issue of red mud accumulation and emissions. This study proposes a “calcification-potash alkali”(CPA) process, wherein potash is utilized instead of sodium alkali to simulate the hydrothermal leaching of kaolinite, the primary silicon-containing mineral phase in bauxite, during the Bayer process. The transformation product is Kaliophilite(KAlSiO4), which can be used to prepare mineral-based silicon‑potassium fertilizers. This paper investigates the dissolution behavior and mechanism of kaolinite during the leaching process. Leaching experiments and analyses (FTIR, XRD, XRF, XPS, and SEM-EDS) reveal that potassium oxide concentration and alkali leaching temperature are the main factors influencing kaolinite transformation. The optimal dissolution conditions are a temperature of 200 °C, a calcium-to‑silicon ratio of 0.2, a K2O concentration of 160 g/L, and a reaction time of 60 min. Under these conditions, the kaolinite reaction rate reaches 98.9 %, yielding potassium aluminosilicate. Furthermore, the heavy metal content and other indices met relevant standards, allowing for its incorporation into organic matter and the preparation of mineral silica‑potassium fertilizers to partially replace industrial fertilizers in agriculture, offering significant cost advantages and promising market prospects. This process transforms the silicon-containing mineral phase in bauxite from waste into a valuable resource, offering a new reference for the utilization of medium- and low-grade bauxite as well as the treatment of red mud.
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来源期刊
Applied Clay Science
Applied Clay Science 地学-矿物学
CiteScore
10.30
自引率
10.70%
发文量
289
审稿时长
39 days
期刊介绍: Applied Clay Science aims to be an international journal attracting high quality scientific papers on clays and clay minerals, including research papers, reviews, and technical notes. The journal covers typical subjects of Fundamental and Applied Clay Science such as: • Synthesis and purification • Structural, crystallographic and mineralogical properties of clays and clay minerals • Thermal properties of clays and clay minerals • Physico-chemical properties including i) surface and interface properties; ii) thermodynamic properties; iii) mechanical properties • Interaction with water, with polar and apolar molecules • Colloidal properties and rheology • Adsorption, Intercalation, Ionic exchange • Genesis and deposits of clay minerals • Geology and geochemistry of clays • Modification of clays and clay minerals properties by thermal and physical treatments • Modification by chemical treatments with organic and inorganic molecules(organoclays, pillared clays) • Modification by biological microorganisms. etc...
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