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Zeolites prepared from calcined and mechanically modified kaolins A comparative study
Kaoliniferous sand and washed industrial kaolin obtained from it were calcined (750 degree C) or milling prior to activation with NaOH. The changes were characterized by pH, cation exchange capacity (CEC), water capacity after calcination (WCC), particle size distribution (PSD) and specific surface...
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Published in: | Applied clay science 2010-07, Vol.49 (3), p.239-246 |
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creator | SAN CRISTOBAL, A. G CASTELLO, R LUENGO, M. A. Martín VIZCAYNO, C |
description | Kaoliniferous sand and washed industrial kaolin obtained from it were calcined (750 degree C) or milling prior to activation with NaOH. The changes were characterized by pH, cation exchange capacity (CEC), water capacity after calcination (WCC), particle size distribution (PSD) and specific surface area (S sub(BET)), as well as by X-ray diffraction (XRD), Fourier transform infrared (FTIR), thermal methods (TGA and DTA), and scanning and transmission electron microscopy (SEM and TEM). Alkali activation of thermally or mechanically modified kaolin increased the cation exchange capacity from 2.4 to 292.8 and from 3.0 to 279.9 cmol kg super(-) super(1) (samples WT and WM respectively). Alkali activation of mechanically modified kaoliniferous sand (OMA), and thermally and mechanically modified washed kaolin (WTA and WMA), yielded zeolite A. An unnamed zeolite, forming microspheres of 0.8-2.3 mu m in size, was also formed in mechanically modified kaoliniferous sand (OMA), washed kaolin (WA) and calcined washed kaolin (WTA) after alkali-activation. Structural disorder in the mechanically modified washed kaolin (WMA) favored the formation of a single type of zeolite. |
doi_str_mv | 10.1016/j.clay.2010.05.012 |
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G ; CASTELLO, R ; LUENGO, M. A. Martín ; VIZCAYNO, C</creator><creatorcontrib>SAN CRISTOBAL, A. G ; CASTELLO, R ; LUENGO, M. A. Martín ; VIZCAYNO, C</creatorcontrib><description>Kaoliniferous sand and washed industrial kaolin obtained from it were calcined (750 degree C) or milling prior to activation with NaOH. The changes were characterized by pH, cation exchange capacity (CEC), water capacity after calcination (WCC), particle size distribution (PSD) and specific surface area (S sub(BET)), as well as by X-ray diffraction (XRD), Fourier transform infrared (FTIR), thermal methods (TGA and DTA), and scanning and transmission electron microscopy (SEM and TEM). Alkali activation of thermally or mechanically modified kaolin increased the cation exchange capacity from 2.4 to 292.8 and from 3.0 to 279.9 cmol kg super(-) super(1) (samples WT and WM respectively). Alkali activation of mechanically modified kaoliniferous sand (OMA), and thermally and mechanically modified washed kaolin (WTA and WMA), yielded zeolite A. An unnamed zeolite, forming microspheres of 0.8-2.3 mu m in size, was also formed in mechanically modified kaoliniferous sand (OMA), washed kaolin (WA) and calcined washed kaolin (WTA) after alkali-activation. 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Alkali activation of mechanically modified kaoliniferous sand (OMA), and thermally and mechanically modified washed kaolin (WTA and WMA), yielded zeolite A. An unnamed zeolite, forming microspheres of 0.8-2.3 mu m in size, was also formed in mechanically modified kaoliniferous sand (OMA), washed kaolin (WA) and calcined washed kaolin (WTA) after alkali-activation. Structural disorder in the mechanically modified washed kaolin (WMA) favored the formation of a single type of zeolite.</description><subject>Activation</subject><subject>Cation exchanging</subject><subject>Disorders</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Kaolin</subject><subject>Mineralogy</subject><subject>Roasting</subject><subject>Sand</subject><subject>Scanning electron microscopy</subject><subject>Silicates</subject><subject>Specific surface</subject><subject>Zeolites</subject><issn>0169-1317</issn><issn>1872-9053</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNotj0lLBDEQhYMoOI7-AU-5iKduU0mvx2FwgwEvzsVLU9kwY3ox6RH63xtxTo969b16FCG3wHJgUD0ccuVxyTlLBitzBvyMrKCpedayUpyTVYLaDATUl-QqxgNLRFO2K7L_MKN3s4l0CmbCYDS1YeypQq_ckCYcNO2N-sTBJc8vtB-1sy5tvjAlh0g3VI19iuLsfgyN81Ev1-TCoo_m5qRrsn96fN--ZLu359ftZpdNHOo5q3lbW2ltKxVrpNDSNMC0rPBPsYBaGSi0qJBB0bQcGym5MqLgQvNCl6VYk_v_u1MYv48mzl3vojLe42DGY-zqinFIJZDIuxOJMf1hAw7KxW4KrsewdFywqmKCi19GvWNm</recordid><startdate>20100701</startdate><enddate>20100701</enddate><creator>SAN CRISTOBAL, A. 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Alkali activation of thermally or mechanically modified kaolin increased the cation exchange capacity from 2.4 to 292.8 and from 3.0 to 279.9 cmol kg super(-) super(1) (samples WT and WM respectively). Alkali activation of mechanically modified kaoliniferous sand (OMA), and thermally and mechanically modified washed kaolin (WTA and WMA), yielded zeolite A. An unnamed zeolite, forming microspheres of 0.8-2.3 mu m in size, was also formed in mechanically modified kaoliniferous sand (OMA), washed kaolin (WA) and calcined washed kaolin (WTA) after alkali-activation. Structural disorder in the mechanically modified washed kaolin (WMA) favored the formation of a single type of zeolite.</abstract><cop>Kidlington</cop><pub>Elsevier</pub><doi>10.1016/j.clay.2010.05.012</doi><tpages>8</tpages></addata></record> |
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subjects | Activation Cation exchanging Disorders Earth sciences Earth, ocean, space Exact sciences and technology Kaolin Mineralogy Roasting Sand Scanning electron microscopy Silicates Specific surface Zeolites |
title | Zeolites prepared from calcined and mechanically modified kaolins A comparative study |
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