Journal of the Clay Science Society of Japan (in Japanese)
Online ISSN : 2186-3563
Print ISSN : 0470-6455
ISSN-L : 0470-6455
Artificial Transformation of Ground Talc into Kaolinite and Smectites by Al-salt solution
Takabumi SAKAMOTOAtsushi YAMAZAKIShoichi KOBAYASHI
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1999 Volume 38 Issue 3 Pages 197-206

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Abstract

Talc has been known as a low reactive mineral under hydrothermal conditions in comparison with the other clays. However, it was expected that grinding treatment increase its reactivity by so-called mechanochemical effect.
In the present study, naturally occurred talc from China was ground in vibrating mill to X-ray amorphous state. The ground talc was then treated hydrothermally with aluminum salts solution for various Al (in reaction systems)/Si (in ground talc) molecular ratios ranging from 0.1 to 2.0. The products were examined by means of X-ray diffractometry, thermal analysis, and infrared absorption spectroscopy.
It was found that the ground talc is successively converted to trioctahedral smectite, dioctahedral smectite, and kaolinite with increasing the Al/Si ratios, by treatment with acidic aluminum bearing solution such as AlCl3, Al2(S04)3, and Al (NO3)3. Al24O11(OH)44Cl6 phase and alunite were also formed as the coproducts in the way of AlCl3 and Al2(SO4)3 solution treatment, respectively.
On the other hand, by the treatment with NaAlO2, the ground talc changed to a trioctahedral smectite and an analcime at low Al/Si ratios, but a serpentine and a hydroxysodalite were formed at high Al/Si ratios. In these cases, the reaction was proceeded in basic condition, and the pH value was increased with increasing of the Al/Si ratios.
It is concluded that grinding significantly increases the hydrothermal reactivity of talc, and the hydrothermal products of the ground talc are controlled by the Si/Al ratio and pH value in reaction system.

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