MORPHOLOGY OF KAOLINITE CRYSTALS SYNTHESIZED UNDER HYDROTHERMAL CONDITIONS

被引:36
作者
FIORE, S [1 ]
HUERTAS, FJ [1 ]
HUERTAS, F [1 ]
LINARES, J [1 ]
机构
[1] CSIC,ESTAC EXPTL ZAIDIN,E-18008 GRANADA,SPAIN
关键词
CRYSTAL GROWTH; ELECTRON MICROSCOPY; KAOLINITE; LATHS; MORPHOLOGY; PLATES; SPHERULES; SYNTHESIS;
D O I
10.1346/CCMN.1995.0430310
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
Scanning electron microscopy has revealed the presence of spherical, lath and platy kaolinite in gels with Si/Al atomic ratio ranging from 1.84 to 0.76 that are hydrothermally treated under different temperature and time conditions. Hemispherical structures and excavated zones, at different stages of evolution, have been observed on the surface of the gel grains, indicating that spherical particles do not precipitate from the solution but are generated from the gels. The quantity of spherical particles depends on temperature, time and the chemical composition of the starting gel. Products from starting material with Si/Al approximate to 1 yield the highest quantity of these particles. Being metastable, sphere dissolution controls the chemistry of the solution and consequently the morphology of the precipitating crystals thus producing more elongated, curved and irregular outlines when gels with Si/Al approximate to 1 are hydrothermally treated.
引用
收藏
页码:353 / 360
页数:8
相关论文
共 26 条
  • [1] Cloos P., Leonard A.J., Moreau J.P., Herbillon A., Fripiat J.J., Structural organization in amorphous silico-aluminas, Clays & Clay Miner, 17, pp. 279-287, (1969)
  • [2] De Kimpe C., Gastuche M.C., Brindley G.W., Low temperature synthesis of clay minerals, Am. Mineral, 49, pp. 1-16, (1964)
  • [3] Eggleton R.A., Non crystalline Fe-Si-Al-oxyhydrox-ides, Clays & Clay Miner, 35, pp. 29-37, (1987)
  • [4] Eggleton R.A., Keller J., The palagonitization of limburgite glass-A TEM study, N. Jb. Miner Mh. Jg, 1982, pp. 321-336, (1982)
  • [5] Espiau P., Pedro G., Comportement des ions aluminiques et de la silice en solution: Etude de la formation de la kaolinite, Clay Miner, 19, pp. 615-627, (1984)
  • [6] Fiore S., The occurrences of smectite and illite in a pyroclastic deposit prior to weathering: Implications on the genesis of 2: 1 clay minerals in volcanic soils, Appl. Clay Sci, 8, pp. 249-259, (1993)
  • [7] Huertas F.J., Sintesis hidrotermal de caolinita, (1991)
  • [8] Huertas F.J., Huertas F., Linares J., Hydrothermal synthesis of kaolinite: Method and characterization of synthetic materials, Appl. Clay Sci, 7, pp. 345-356, (1993)
  • [9] Huertas F.J., Huertas F., Linares J., A new approach to kinetics of kaolinite synthesis, Proc. 4th Int. Symposium on Hydrothermal Reaction, pp. 87-90, (1993)
  • [10] Keller W.D., Scan electron micrograph of kaolins collected from diverse environments of origin-I, Clays & Clay Miner, 24, pp. 107-113, (1976)