Interzeolite Transformation through Cross-Nucleation: A Molecular Mechanism for Seed-Assisted Synthesis

被引:3
|
作者
Chu-Jon, Carlos [1 ]
Martinez, Eli [1 ]
Bertolazzo, Andressa A. [1 ,5 ]
Banik, Suvo [2 ,3 ]
Rimer, Jeffrey D. [4 ]
Sankaranarayanan, Subramanian K. R. S. [2 ,3 ]
Molinero, Valeria [1 ]
机构
[1] Univ Utah, Dept Chem, Salt Lake City, UT 84112 USA
[2] Univ Illinois, Dept Mech & Ind Engn, Chicago, IL 60607 USA
[3] Argonne Natl Lab, Ctr Nanoscale Mat, Lemont, IL 60439 USA
[4] Univ Houston, Dept Chem & Biomol Engn, Houston, TX 77204 USA
[5] Weber State Univ, Dept Chem & Biochem, Ogden, UT 84408 USA
关键词
MONTE-CARLO SIMULATIONS; ZEOLITE; SILICA; POLYMERIZATION; CONVERSION; STABILITY; CRYSTALS; DYNAMICS; MODEL; ABC-6;
D O I
10.1021/jacs.4c12863
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Polymorph selection and efficient crystallization are central goals in zeolite synthesis. Crystalline seeds are used for both purposes. While it has been proposed that zeolite seeds induce interzeolite transformation by dissolving into structural units that promote nucleation of the daughter crystal, the seed's structural elements do not always match those of the target zeolite. This discrepancy raises the question of how the seed promotes the daughter phase. Here, we present the first molecularly resolved investigation of seed-assisted zeolite synthesis. Using molecular simulations, we reproduce the experimental finding that a parent zeolite can promote the nucleation of a daughter zeolite even when it lacks common composite building units (CBUs) or crystal planes. Modeling the seed-assisted synthesis of an AFI-type zeolite using zeolite CHA, our simulations indicate that stand-alone CBUs from the parent seed do not facilitate daughter crystal formation. However, introducing the intact seed significantly reduces the synthesis time, supporting that seed integrity is key to increased efficiency. This reduction arises from the cross-nucleation of the AFI-type zeolite on the CHA (001) face. We find that parent and daughter zeolites are connected by an interfacial transition layer with an order distinct from that of both zeolites. Simulations reveal that cross-nucleation occurs over a broad range of synthesis conditions. We argue that cross-nucleation would be most favorable for zeolite pairs that share crystalline planes such as those forming intergrowths. Our findings suggest that the prevalence of intergrowths with a common lattice plane in zeolite synthesis is likely a kinetic effect of accelerated cross-nucleation.
引用
收藏
页码:33204 / 33213
页数:10
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