Surface and porosity of nanocrystalline boehmite xerogels

被引:32
作者
Alphonse, P [1 ]
Courty, M [1 ]
机构
[1] Univ Toulouse 3, CIRIMAT, UMR CNRS 5085, F-31062 Toulouse, France
关键词
boehmite; specific surface area; porosity; PSD; comparative plot;
D O I
10.1016/j.jcis.2005.04.013
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
Boehmite xerogels are prepared by hydrolysis of Al(OC4H9)(3) followed by peptization with HNO3 (H+/Al = 0, 0.07, 0.2). XRD and TEM show that these gels are made of nanosized crystals (5-9 nm in width and 3 nm thick). According to the amount of acid, no significant differences are found in size and shape, but only in the spatial arrangement of the crystallites. Nitrogen adsorption-desorption isotherms of nonpeptized gels are of type IV, whereas isotherms of peptized gels are of type I. These isotherms are analyzed by the t-plot method. The majority of pore volume results from intercrystalline mesopores, but the peptized gels also contain intercrystalline micropores. The particle packing is very dense for the gel peptized with H+/Al = 0.2 (porosity = 0.26), but it is less dense in non-peptized get (porosity = 0.44). Heating these gels under vacuum creates, from 250 degrees C onwards, an intracrystalline microporosity resulting from the conversion of boehmite into transition alumina. But heating also causes intercrystalline micropores collapsing. The specific surface area increases up to a limit temperature (300 degrees C for nonpeptized gels and 400 degrees C for peptized) beyond which sintering of the particles begins and the surface decreases. The PSD are calculated assuming a cylindrical pore geometry and using the corrected Kelvin equation proposed by Kruk et al. Peptized xerogels give a monomodal distribution with a maximum near 2 nm and no pores are larger than 6 nm. Nonpeptized gels have a bimodal distribution with a narrow peak near to 2 nm and a broad unsymmetrical peak with a maximum at 4 nm. Heating in air above 400 degrees C has a strong effect on the porosity. As the temperature increases, there is a broadening of the distribution and a marked decrease of small pores (below 3 nm). However, even after treatment at 800 degrees C, micropores are still present. (c) 2005 Elsevier Inc. All rights reserved.
引用
收藏
页码:208 / 219
页数:12
相关论文
共 41 条
[11]   CRYSTAL-STRUCTURE OF BOEHMITE [J].
CHRISTOPH, GG ;
CORBATO, CE ;
HOFMANN, DA ;
TETTENHORST, RT .
CLAYS AND CLAY MINERALS, 1979, 27 (02) :81-86
[12]  
De Boer JH, 1958, Colston Pap, V10, P68
[13]   Influence of aqueous solution chemistry on the surface charge, viscosity and stability of concentrated alumina dispersions in water [J].
Evanko, CR ;
Delisio, RF ;
Dzombak, DA ;
Novak, JW .
COLLOIDS AND SURFACES A-PHYSICOCHEMICAL AND ENGINEERING ASPECTS, 1997, 125 (2-3) :95-107
[14]   *ETUDE CINETIQUE DE LA DISSOCIATION THERMIQUE DHYDRATES DALUMINE [J].
EYRAUD, C ;
GOTON, R .
JOURNAL DE CHIMIE PHYSIQUE ET DE PHYSICO-CHIMIE BIOLOGIQUE, 1954, 51 (09) :430-433
[15]  
Fauchadour D, 2002, STUD SURF SCI CATAL, V143, P453
[16]  
German R.M., 1989, PARTICLE PACKING CHA
[17]   Thermal study of a precursor for catalyst supports: Well- and micro-crystallised boehmites [J].
Gobichon, AE ;
Rebours, B ;
Euzen, P .
EPDIC 7: EUROPEAN POWDER DIFFRACTION, PTS 1 AND 2, 2001, 378-3 :523-528
[18]  
GREGG SJ, 1982, ADSORPTION SURFACE
[19]   HEATS OF ADSORPTION OF WATER ON ALPHA-ALUMINA AND GAMMA-ALUMINA [J].
HENDRIKS.BA ;
RUDHAM, R ;
PEARCE, DR .
JOURNAL OF CATALYSIS, 1972, 24 (01) :82-&
[20]   Physicochemical foundations for characterization of adsorbents by using high-resolution comparative plots [J].
Jaroniec, M ;
Kaneko, K .
LANGMUIR, 1997, 13 (24) :6589-6596