Understanding the dissolution of zeolites

被引:94
作者
Hartman, Ryan L. [1 ]
Fogler, H. Scott [1 ]
机构
[1] Univ Michigan, Dept Chem Engn, Ann Arbor, MI 48109 USA
关键词
D O I
10.1021/la063699g
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Scientific knowledge of how zeolites, a unique classification of microporous aluminosilicates, undergo dissolution in aqueous hydrochloric acid solutions is limited. Understanding the dissolution of zeolites is fundamental to a number of processes occurring in nature and throughout industry. To better understand the dissolution process, experiments were carried out establishing that the Si-to-Al ratio controls zeolite framework dissolution, by which the selective removal of aluminum constrains the removal of silicon. Stoichiometric dissolution is observed for Type 4A zeolite in HCl where the Si-to-Al ratio is equal to 1.0. Framework silicon dissolves completely during Type 4A dissolution and is followed by silicate precipitation. However, for the zeolite analcime which has a Si-to-Al ratio of 2.0 dissolves non-stoichiometrically as the selective removal of aluminum results in partially dissolved silicate particles followed by silicate precipitation. In Type Y zeolite, exhibiting a Si-to-Al ratio of 3.0, there is insufficient aluminum to weaken the structure and cause silicon to dissolve in HCl. Thus, little or no precipitation is observed, and amorphous undissolvable silicate particles remain intact. The initial dissolution rates of Type Y and 4A zeolites demonstrate that dissolution is constrained by the number of available reaction sites, and a selective removal rate parameter is applied to delineate the mechanism of particle dissolution by demonstrating the kinetic influence of the Si-to-Al ratio. Zeolite framework models are constructed and used to undergird the basic dissolution mechanism. The framework models, scanning electron micrographs of partially dissolved crystals, and experimentally measured dissolution rates all demonstrate that a zeolite's Si-to-Al framework ratio plays a universal role in the dissolution mechanism, independent of framework type. Consequently, the unique mechanism of zeolite dissolution has general implications on how petroleum reservoir stimulation treatments should be designed.
引用
收藏
页码:5477 / 5484
页数:8
相关论文
共 41 条
[11]   DISSOLUTION OF HIGH-SILICA ZEOLITES IN ALKALINE-SOLUTIONS .1. DISSOLUTION OF SILICALITE-1 AND ZSM-5 WITH DIFFERENT ALUMINUM CONTENT [J].
CIZMEK, A ;
SUBOTIC, B ;
AIELLO, R ;
CREA, F ;
NASTRO, A ;
TUOTO, C .
MICROPOROUS MATERIALS, 1995, 4 (2-3) :159-168
[12]   ACID STRENGTH AND ALUMINUM SITE REACTIVITY OF Y ZEOLITES [J].
DEMPSEY, E .
JOURNAL OF CATALYSIS, 1974, 33 (03) :497-499
[13]  
Dyer A., 1988, INTRO ZEOLITE MOL SI
[14]   The chemical behavior of natural zeolites in aqueous environments: Interactions between low-silica zeolites and 1 M NaCl solutions of different initial pH-values [J].
Filippidis, A ;
Godelitsas, A ;
Charistos, D ;
Misaelides, P ;
KassoliFournaraki, A .
APPLIED CLAY SCIENCE, 1996, 11 (2-4) :199-209
[15]   Synthesis and organization of zeolite-like materials with three-dimensional helical pores [J].
Gier, TE ;
Bu, XH ;
Feng, PY ;
Stucky, GD .
NATURE, 1998, 395 (6698) :154-157
[16]   Reaction kinetics and mechanisms of zeolite dissolution in hydrochloric acid [J].
Hartman, RL ;
Fogler, HS .
INDUSTRIAL & ENGINEERING CHEMISTRY RESEARCH, 2005, 44 (20) :7738-7745
[17]  
HARTMAN RL, 2006, THESIS U MICHIGAN AN
[18]   The unique mechanism of analcime dissolution by hydrogen ion attack [J].
Hartman, Ryan L. ;
Fogler, H. Scott .
LANGMUIR, 2006, 22 (26) :11163-11170
[19]  
Iler RK, 1979, CHEM SILICA SOLUBILI, DOI DOI 10.1002/ANGE.19800920433
[20]   Evaluation of the secondary pore structure of hydrothermally- and acid-treated faujasite type zeolites [J].
Kawai, T ;
Tsutsumi, K .
ADSORPTION-JOURNAL OF THE INTERNATIONAL ADSORPTION SOCIETY, 1998, 4 (3-4) :225-231