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皂石的异相水热合成及其影响因素
Heterogeneous Hydrothermal Synthesis of Saponite and Factors Affecting its Crystallinity

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张旦 1   何宏平 1   陶奇 1 *   陈漫游 1   吉世超 1   李甜 2  
文摘 与均相水热反应相比,异相水热反应不仅可以提供一个骨架离子的适度过饱和环境,而且其新相成核所需逾越的能垒较低,更有利于晶体的形成和生长。本文采用异相水热法合成在皂石,即固定初始物料中氧化镁的添加量与硅、铝的添加量之和的摩尔比为一定值,n(Mg)/n(Si+Al) =3∶4],在不同的合成温度和时间条件下合成了一系列不同Si/Al比的样品。所有样品的XRD图均呈现层状硅酸盐矿物的特征衍射峰,且d_((060))≥0.153 nm,说明合成的是皂石矿物。其中,当n(Si)/n(Al)=5.43~7.89时,皂石的结晶度较好。实验表明,延长时间、提高合成温度有利于皂石晶体生长。在较低温度(160℃)下,样品中的杂相主要为水镁石和方沸石。水镁石相的存在主要归因于氧化镁在碱性条件下的快速水合及水镁石的慢速溶解,而方沸石则是由于Mg~(2+)释放缓慢,导致溶液中Si~(4+)及Al~(3+)相对过剩而形成。这两种杂相均会随着反应时间的延长而逐渐消失。在较高温度(300 ℃)下,皂石的结晶度明显升高,并由于Mg~(2+)的快速释放导致Mg~(2+)的局部过剩,因而形成了少量1∶1型的纤蛇纹石。
其他语种文摘 Compared with homogeneous synthesis technology, heterogeneous synthesis can promote the nucleation and subsequently accelerate the growth of secondary minerals by providing a local environment with super-saturation of ion concentration and a relatively lower energy barrier. In the present study, a series of samples were synthesized by altering Si/Al ratio (fixing the Mg/(Si+Al) =3∶4), reaction temperature and time. Characteristic reflections of phyllosilicate were recorded in XRD patterns of the resulting products with d_((060))≥0.153 nm, indicating a successful synthesis of saponite. The well-crystallized saponite was obtained in the initial Si/Al ratio range of 5.43-7.89, and their crystallinities increased with increasing reaction temperature and time. At a temperature of 160℃, brucite and analcime formed as impurities, resulting from the low dissolution ability of brucite and the excess of Si~(4+) and Al~(3+) in the solution. Both of them disappeared with extension of reaction time. At a temperature of 300℃, a small amount of chrysotile was formed, corresponding to the rapid release of Mg~(2+).
来源 矿物学报 ,2016,36(2):241-246 【核心库】
DOI 10.16461/j.cnki.1000-4734.2016.02.011
关键词 皂石 ; 异相水热合成 ; 影响因素 ; 纤蛇纹石
地址

1. 中国科学院广州地球化学研究所, 中国科学院矿物学与成矿学重点实验室;;广东省矿物物理与材料研究开发重点实验室, 广东, 广州, 510640  

2. 中国科学院广州地球化学研究所, 中国科学院矿物学与成矿学重点实验室, 广东, 广州, 510640

语种 中文
文献类型 研究性论文
ISSN 1000-4734
学科 地质学
基金 国家自然科学基金-广东联合基金 ;  国家自然科学基金
文献收藏号 CSCD:5720495

参考文献 共 18 共1页

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引证文献 2

1 陈漫游 固体核磁光谱法研究镁铝复合氧化物的水热转化机制 岩石矿物学杂志,2017,36(6):887-893
被引 1

2 何宏平 矿物结构与矿物物理研究进展综述(2011~ 2020年) 矿物岩石地球化学通报,2020,39(4):697-713
被引 5

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