Combined NMR, SAXS, and DLS study of concentrated clear solutions used in silicalite-1 zeolite synthesis

被引:77
作者
Aerts, Alexander
Follens, Lana R. A.
Haouas, Mohamed
Caremans, Tom P.
Delsuc, Marc-Andre
Loppinet, Benoit
Vermant, Jan
Goderis, Bart
Taulelle, Francis
Martens, Johan A.
Kirschhock, Christine E. A.
机构
[1] Katholieke Univ Leuven, Ctr Surface Chem & Catalysis, B-3001 Heverlee, Belgium
[2] Univ Versailles, Inst Lavoisier, F-78035 Versailles, France
[3] FORTH, IESL, GR-71110 Iraklion, Greece
[4] Ctr Biochim Struct, F-34090 Montpellier, France
[5] Katholieke Univ Leuven, Dept Chem Engn, B-3001 Heverlee, Belgium
[6] Katholieke Univ Leuven, Dept Chem, B-3001 Heverlee, Belgium
关键词
D O I
10.1021/cm070693j
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
Concentrated clear solutions, as used for the preparation of Silicalite-1 zeolite, were synthesized from tetrapropylammonium hydroxide, tetraethylorthosilicate, and water. The solutions were analyzed using three techniques: quantitative Si-29 NMR, synchrotron small-angle X-ray scattering (SAXS), and dynamic light scattering (DLS). Si-29 NMR showed the coexistence of silicate oligomers and particles. For the first time, both fractions were analyzed simultaneously, providing a global, quantitative description of the clear solution microstructure. The SAXS patterns, typical of interacting particles, could be used together with the Si-29 NMR deduced particle volume fraction to estimate a particle size. A careful analysis of DLS data of the dynamics of the suspensions revealed the occurrence of two diffusive processes. The faster process is a collective particle diffusion. The slower process corresponds to the particle self-diffusion and is present because of the presence of polydispersity in size, shape, and/or surface charge. The self-diffusion coefficient provides a means to estimate the equivalent hydrodynamic radius. The observations hence reveal a complex, polydisperse mixture of particles present at the onset of the Silicalite-1 zeolite formation. Implications on the proposed zeolite formation mechanisms are briefly discussed.
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页码:3448 / 3454
页数:7
相关论文
共 27 条
[1]   Self-diffusion and collective diffusion of charged colloids studied by dynamic light scattering [J].
Appell, J ;
Porte, G ;
Buhler, E .
JOURNAL OF PHYSICAL CHEMISTRY B, 2005, 109 (27) :13186-13194
[2]   MECHANISMS OF STRUCTURE DIRECTION IN THE SYNTHESIS OF PURE-SILICA ZEOLITES .1. SYNTHESIS OF TPA/SI-ZSM-5 [J].
BURKETT, SL ;
DAVIS, ME .
CHEMISTRY OF MATERIALS, 1995, 7 (05) :920-928
[3]   29Si NMR studies of zeolite precursor solutions [J].
Cheng, CH ;
Shantz, DF .
JOURNAL OF PHYSICAL CHEMISTRY B, 2006, 110 (01) :313-318
[4]   Small-angle scattering studies of silicalite-1 growth from clear solutions [J].
Cheng, CH ;
Shantz, DF .
CURRENT OPINION IN COLLOID & INTERFACE SCIENCE, 2005, 10 (5-6) :188-194
[5]   The hydrothermal synthesis of zeolites: Precursors, intermediates and reaction mechanism [J].
Cundy, CS ;
Cox, PA .
MICROPOROUS AND MESOPOROUS MATERIALS, 2005, 82 (1-2) :1-78
[6]   Mechanistic principles of nanoparticle evolution to zeolite crystals [J].
Davis, TM ;
Drews, TO ;
Ramanan, H ;
He, C ;
Dong, JS ;
Schnablegger, H ;
Katsoulakis, MA ;
Kokkoli, E ;
McCormick, AV ;
Penn, RL ;
Tsapatsis, M .
NATURE MATERIALS, 2006, 5 (05) :400-408
[7]   Maximum entropy processing of DOSY NMR spectra [J].
Delsuc, MA ;
Malliavin, TE .
ANALYTICAL CHEMISTRY, 1998, 70 (10) :2146-2148
[8]   Formation and structure of self-assembled silica nanoparticles in basic solutions of organic and inorganic cations [J].
Fedeyko, JM ;
Vlachos, DG ;
Lobo, RF .
LANGMUIR, 2005, 21 (11) :5197-5206
[9]  
Kirschhock C. E., 2001, ANGEW CHEM, V113, P2707
[10]   Identification of precursor species in the formation of MFI zeolite in the TPAOH-TEOS-H2O system [J].
Kirschhock, CEA ;
Ravishankar, R ;
Verspeurt, F ;
Grobet, PJ ;
Jacobs, PA ;
Martens, JA .
JOURNAL OF PHYSICAL CHEMISTRY B, 1999, 103 (24) :4965-4971