Calcium oxides for CO2 capture obtained from the thermal decomposition of CaCO3 particles coprecipitated with Al3+ ions

被引:16
|
作者
Beruto, D. T. [1 ,2 ]
Botter, R. [1 ,2 ]
Lagazzo, A. [2 ]
Finocchio, E. [2 ]
机构
[1] Univ Genoa, Res Ctr Mat Sci & Eng, I-16129 Genoa, GE, Italy
[2] Univ Genoa, Dept Chem Engn & Proc, Fac Engn, I-16129 Genoa, Italy
关键词
Limestone decomposition; Sintering; CO2; capture; Al ions; Dilatometer; CAO-BASED SORBENT; FLUIDIZED-BED; CARBONATION; THERMODYNAMICS; CHEMISORPTION; SEQUESTRATION; TEMPERATURE; COMBUSTION; KINETICS; SURFACE;
D O I
10.1016/j.jeurceramsoc.2011.08.022
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
Calcium-carbonate powders were coprecipitated with Al3+ and then decomposed in air and/or under a CO2 flux between 590 degrees C and 1150 degrees C. The data were analysed using a consecutive-decomposition-dilatometer method and the kinetic results were discussed according to the microstructure analysis done by N-2 adsorption isotherms (78 K), SEM and FT-IR measurements. Below 1000 degrees C, CaCO3 particle thermal-decomposition was pseudomorphic, resulting in the formation of a CaO grain porous network. When the CaO grains were formed, the Al3+ diffused among them, producing AlO4 groups that promoted the CaO grain coarsening and reduced O-2(-) surface sites available to CO2 adsorbed molecules to form CO32-. In pure CaO, CO32- diffused through the grain boundary, enhancing Ca2+ and O-2(-) mobility; AlO4 groups reduced CO32- penetration and CaO sintering rate. Above 1000 degrees C, the sintering rate of the doped samples exceeded that of the undoped, likely because of Al3+ diffusion in CaO and viscous flow. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:307 / 315
页数:9
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