Transactions of Nonferrous Metals Society of China The Chinese Journal of Nonferrous Metals

您目前所在的位置:首页 - 期刊简介 - 详细页面

中国有色金属学报

ZHONGGUO YOUSEJINSHU XUEBAO

第18卷    第z1期    总第100期    2008年6月

[PDF全文下载]        

    

文章编号:1004-0609(2008)S1-0172-11
硅矿物在拜耳法溶出中的行为
赵清杰1, 2,杨巧芳1,陈启元2,尹周澜2,吴争平2,殷振国3

(1. 中国铝业股份有限公司 郑州研究院,郑州  450041;2. 中南大学 化学化工学院,长沙  410083;
3. 深圳市海盈科技有限公司,深圳  518104
)

摘 要: 研究了高岭石、伊利石、叶蜡石等几种单体硅矿物在铝酸钠溶液中的溶出行为。结果表明,高岭石、伊利石、叶蜡石等单体硅矿物在铝酸钠溶液中的溶出速率受温度等反应条件的影响。采用量子化学理论计算,用CASTEP程序模块,在GGA-PW91基组水平,对高岭石、伊利石、叶蜡石及其常见完全解理面(001)slab模型进行几何优化,揭示了高岭石、伊利石、叶蜡石在铝酸钠溶液中反应活性差异的微观本质。高岭石、伊利石和叶蜡石的反应活性存在较明显的不同,其中叶蜡石的反应活性最大。伊利石的Si—O键结合力最强,Al—O键结合力相对最弱,相对最难反应脱Si;叶蜡石Si—O键结合力相对最弱,相对较容易反应脱除Si。OH的存在对高岭石、伊利石、叶蜡石完全解理面的微观电子结构、Si—O键的结合力等均影响显著,其中OH对高岭石表面性质及    Si—O键结合力的降低产生的影响最大,因此高岭石在相对较低温度下较易在碱性溶液中反应脱硅。

 

关键字: 硅矿物;氧化铝;拜耳法溶出;铝酸钠溶液;反应活性;行为

Behavior of silicon minerals during Bayer digestion
ZHAO Qing-jie1, 2, YANG Qiao-fang1, CHEN Qi-yuan2, YIN Zhou-lan2, WU Zheng-ping2, YIN Zhen-guo3

1. Zhengzhou Research Institute, Aluminum Corporation of China Limited, Zhengzhou 450041, China;
2. School of Chemistry and Chemical Engineering, Central South University, Changsha 410083, China;
3. Shenzhen Herewin Technology Co., Ltd, Shenzhen 518140, China

Abstract:The digestion behaviors of several mono-silicon minerals including kaolinite, illite, pyrophyllite in aluminate solution were investigated. The results show that the digestion rate of kaolinite, illite and pyrophyllite in aluminate solution is influenced by reaction conditions such as temperature. By adopting quantum chemistry theoretical calculation, and using CASTEP procedure module, the slab model of kaolinite, illite, pyrophyllite and their ordinary complete cleavage plane (001) are geometry optimized at GGA-PW91 level. The micro-essence of the differenent reaction activity among kaolinite, illite and pyrophyllite in aluminate solution is opened out. The reaction activity of kaolinite, illite and pyrophyllite is obviously different and the reaction activity of pyrophyllite is the highest. The Si—O bond strength of illite is the strongest and its Al—O bond strength is comparatively the most weak, so its Si is the most difficult to remove. The Si—O bond strength of pyrophyllite is the most weak, so its Si is relatively easier to remove. The micro-electron structure of complete cleavage plane and the Si—O bond strength of kaolinite, illite and pyrophyllite are evidently influenced by the existence of OH, of which the surface character and the reduction of Si—O bond strength of kaolinite are influenced most by OH, therefore the desilication of kaolinite in alkaline solution at relatively lower temperature is easier.

 

Key words: silicon minerals; alumina; Bayer digestion; aluminate solution; reaction activity; behavior

ISSN 1004-0609
CN 43-1238/TG
CODEN: ZYJXFK

ISSN 1003-6326
CN 43-1239/TG
CODEN: TNMCEW

主管:中国科学技术协会 主办:中国有色金属学会 承办:中南大学
湘ICP备09001153号 版权所有:《中国有色金属学报》编辑部
------------------------------------------------------------------------------------------
地 址:湖南省长沙市岳麓山中南大学内 邮编:410083
电 话:0731-88876765,88877197,88830410   传真:0731-88877197   电子邮箱:f_ysxb@163.com