首页|钾霞石制备体系碱性滤液的利用技术

钾霞石制备体系碱性滤液的利用技术

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为处理钾长石水热制备钾霞石所产生的碱性滤液,本文采用水热法,考察了氢氧化铝溶解时间、晶化时间、晶化温度、水碱比对钾霞石产率和白度的影响,并对合成钾霞石物相进行了表征.结果表明,合成钾霞石的最佳条件为,氢氧化铝溶解时间为1.5 h,晶化时间为4 h,晶化温度280℃,水碱比为1.8.XRD结果表明,产物为钾霞石粉体.傅里叶变换红外光谱表明,Al(OH)3中的Al在水热条件下进入到Si—O骨架中形成了 Si—O—Al官能团,从而印证了钾霞石的合成.差热分析结果表明,合成钾霞石具有良好的热稳定性.氮气吸附结果表明,合成钾霞石比表面积为5.18 m2/g,平均孔径为32.98 nm.实现了钾长石水热制备钾霞石所剩碱性滤液的资源化利用,并为钾长石水热制备钾霞石提供了一种母液循环的思路,使水热制备钾霞石工业化成为一种可能.
Utilization technology of alkaline filtrate in kaliophilite preparation system
In order to produce alkaline filtrate from potassium feldspar hydrothermal preparation of potassium neph-eline,the effects of dissolution time,crystallization time,crystallization temperature and water-alkali ratio on the yield and whiteness of potassium nepheline were investigated by hydrothermal method.The results show that the optimum conditions for the synthesis of potassium nepheline are as follows:the dissolution time of alumina hydrox-ide is 1.5 hours,the crystallization time is 4 hours,the crystallization temperature is 280℃,and the water-alkali ratio is 1.8.XRD spectrum shows the product is kaliophilite owder.FTIR spectrum shows that Al in Al(OH)3 enters the Si—O framework to form Si—O—Al functional groups under hydrothermal conditions,thus confirming the synthesis of kaliophilite.The result of DTG indicates that the kaliophilite synthesized has good thermal stability.Isotherm indicates that the surface area of synthetic kaliophilite is 5.18 m2/g and the average pore size is 32.98 nm.The alkaline filtrate produced by hydrothermal preparation of potassium nepheline by potassium feldspar was real-ized as resource utilization,and a kind of mother liquor circulation idea was provided for hydrothermal preparation of potassium nepheline by potassium feldspar.The industrialization of hydrothermal preparation of potassium nephe-line has become a possibility.

kaliophilitehydrothermal processaluminum hydroxide

路华龙、霍光祥、段永华、勾明雷、刘军娜、刘晨

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河南科技大学化学化工学院,河南洛阳 471000

钾霞石 水热法 氢氧化铝

河南省重点攻关项目

212102210601

2024

岩石矿物学杂志
中国地质学会岩石学专业委员会 矿物学专业委员会 中国地质科学院地质所

岩石矿物学杂志

CSTPCD北大核心
影响因子:1.104
ISSN:1000-6524
年,卷(期):2024.43(1)
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