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.
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收藏
页码:5477 / 5484
页数:8
相关论文
共 41 条
  • [1] MOLECULAR SIEVE SORBENTS FROM CLINOPTILOLITE
    BARRER, RM
    MAKKI, MB
    [J]. CANADIAN JOURNAL OF CHEMISTRY-REVUE CANADIENNE DE CHIMIE, 1964, 42 (06): : 1481 - &
  • [2] Tailored porous materials
    Barton, TJ
    Bull, LM
    Klemperer, WG
    Loy, DA
    McEnaney, B
    Misono, M
    Monson, PA
    Pez, G
    Scherer, GW
    Vartuli, JC
    Yaghi, OM
    [J]. CHEMISTRY OF MATERIALS, 1999, 11 (10) : 2633 - 2656
  • [3] KINETICS OF QUARTZ DISSOLUTION AT LOW-TEMPERATURES
    BRADY, PV
    WALTHER, JV
    [J]. CHEMICAL GEOLOGY, 1990, 82 (3-4) : 253 - 264
  • [4] Breck D. W., 1984, ZEOLITE MOL SIEVES S
  • [5] Surface science - How minerals react with water
    Brown, GE
    [J]. SCIENCE, 2001, 294 (5540) : 67 - +
  • [6] Large-cage zeolite structures with multidimensional 12-ring channels
    Bu, XH
    Feng, PY
    Stucky, GD
    [J]. SCIENCE, 1997, 278 (5346) : 2080 - 2085
  • [7] Hydrothermal synthesis and structural characterization of zeolite-like structures based on gallium and aluminum germanates
    Bu, XH
    Feng, PY
    Gier, TE
    Zhao, DY
    Stucky, GD
    [J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1998, 120 (51) : 13389 - 13397
  • [8] CARLAND RM, 1988, ACS SYM SER, V368, P292
  • [9] Biomimetic synthesis of ordered silica structures mediated by block copolypeptides
    Cha, JN
    Stucky, GD
    Morse, DE
    Deming, TJ
    [J]. NATURE, 2000, 403 (6767) : 289 - 292
  • [10] Silicatein filaments and subunits from a marine sponge direct the polymerization of silica and silicones in vitro
    Cha, JN
    Shimizu, K
    Zhou, Y
    Christiansen, SC
    Chmelka, BF
    Stucky, GD
    Morse, DE
    [J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 1999, 96 (02) : 361 - 365