Use of 29Si and 27Al MAS NMR to study thermal activation of kaolinites from Brazilian Amazon kaolin wastes

被引:65
|
作者
Barreto Maia, Ana Aurea [1 ]
Angelica, Romulo Simoes [1 ]
Neves, Roberto de Freitas [1 ]
Poellmann, Herbert [2 ]
Straub, Chris [2 ]
Saalwaechter, Kay [2 ]
机构
[1] Fed Univ Para, Programa Posgrad Geol & Geoquim, BR-66075110 Belem, Para, Brazil
[2] Univ Halle Wittenberg, D-06120 Halle, Germany
基金
巴西圣保罗研究基金会;
关键词
Residue; Kaolinite; Metakaolinite; Reactivated; MULLITE REACTION SEQUENCE; CLAY-MINERALS; IRON; DEHYDROXYLATION; TRANSFORMATIONS; CRYSTALLINITY; BENEFICIATION; DECOMPOSITION; DISORDER; DEPOSITS;
D O I
10.1016/j.clay.2013.10.028
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The study of thermal activation of kaolinite at various temperatures to produce highly reactive metakaolinite from Brazilian Amazon kaolin wastes was studied using Al-27 and Si-29 magic angle spinning nuclear magnetic resonance (MAS NMR). The wastes used in the current study came from the Capim and Jari regions in northern Brazil. The mineralogical and chemical characterizations of Jari kaolin (KJ) waste were performed by XRD, FOR, DTA-TGA, SEM and chemical analyses. The results indicate that the Jan and Capim kaolins (KC) wastes are composed primarily of kaolinite and that KJ is composed of a typical kaolinite with a low degree of structural order. The ideal temperature to produce highly reactive metakaolinite is 600 degrees C for KJ and 700 degrees C for KC, suggesting that the degree of structural order of kaolinite has a definite influence on its dehydroxylation temperature. These results were confirmed when zeolite NaA was synthesized from metakaolins produced at temperatures used in this work. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:189 / 196
页数:8
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