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Hydrothermal Synthesis of Clay Minerals from Ground Talc

Research Project

Project/Area Number 07640649
Research Category

Grant-in-Aid for Scientific Research (C)

Allocation TypeSingle-year Grants
Section一般
Research Field Petrology/Mineralogy/Science of ore deposit
Research InstitutionOkayama University of Science

Principal Investigator

SAKAMOTO Takabumi  Okayama University of Science Faculty of Science, Professor, 理学部, 教授 (60098580)

Co-Investigator(Kenkyū-buntansha) KOBAYASHI Shoichi  Kurashiki University of Science and the Arts College of Science and Industrial T, 産業科学技術学部, 助教授 (20109739)
Project Period (FY) 1995 – 1996
Project Status Completed (Fiscal Year 1996)
Budget Amount *help
¥2,300,000 (Direct Cost: ¥2,300,000)
Fiscal Year 1996: ¥700,000 (Direct Cost: ¥700,000)
Fiscal Year 1995: ¥1,600,000 (Direct Cost: ¥1,600,000)
KeywordsClay Minerals / Hydrothermal Synthesis / Talc / Grinding / Smectite / Kaolinite / Sepiolite / セピオライト
Research Abstract

In order to investigate the hydrothermal synthesis of clay minerals, mechanochemically activated ground talc was hydrothermally treated with various salt solutions. Results obtained are as follows ;
1. Talc was changed into X-ray amorphous material by the grinding using a vibrating mill. However, 29Si-NMR data showed that this amorphous material contains a cluster of original layr structure of talc.
2. Tri-octahedral smectite and poorly crystallized talc are formed from the ground talc by the hydrothermal treatment with Na salts (NaOH,Na_2CO_3, NaHCO_3, and NaCl) solutions or distillled water at 200 or 250゚C for 168 hours. However, no sepiolote was obtained.
3. In the Hydrothermal treatment with Al salt (AlCl_3, Al(NO_3)_3, Al_2(SO_4)_3, and NaAlO_2) solutions at 200 or 250゚C for up to 240 hours, products were differed depend on the Al to Si (in the starting material) ratio and pH conditions. In the acidic condition, tri-octahedral smectite was formed in the case of low Al/Si ratio. In the medium Al/Si ratio, di-octahedral smectite was formed. Kaolinite was formed in high Al/Si ratio. On the other hand, tri-octahedral smectite was formed in the low Al/Si ratio and serpentine was obtained in the high Al/Si ratio, in basic condition.

Report

(3 results)
  • 1996 Annual Research Report   Final Research Report Summary
  • 1995 Annual Research Report

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Published: 1995-04-01   Modified: 2016-04-21  

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