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1987 Fiscal Year Final Research Report Summary

Fundanmental Studies of Fibrous Clay Minerals -- Dehydtation Mechanism, Surface Properties, and Acis Treatment.

Research Project

Project/Area Number 60550449
Research Category

Grant-in-Aid for General Scientific Research (C)

Allocation TypeSingle-year Grants
Research Field 資源開発工学
Research InstitutionWaseda University

Principal Investigator

OTSUKA Ryohei  School of Science and Engineering, 理工学部, 教授 (80063204)

Co-Investigator(Kenkyū-buntansha) TSUTSUMI Sadao  School of Education, 教育学部, 教授 (30063613)
Project Period (FY) 1985 – 1987
KeywordsSepiolite / Dehydration Mechanisw / Specific Surface Area / Pore Size Distribution / Cation Exchange Capacity / Acid Treatment / 非晶質繊維状珪酸ゲル
Research Abstract

In order to develope the new unilization of fibrous clay minerals, especially sepiolite, fundamental studied were performed, giving the following results.
1. Dehydration mechanism of sepiolite The structural change of sepiolite due to dehydration, i.e., the forlding of the crystal lattice, occurs homogenecusly over the whole crystal. The rate of the first step dehydration of bound water is controlled by the water separation process from the Mg at the ribbon edge. The rest of the bound water diffuses out from the crystal through the lattice (the secons tep dehydration). The dehydration rate is determined by the water diffusion process in the folded channels.
2. Surface propertied of sepiolite (1) Specific surface areas tange from 443 m^2/g(Imisehir) to 231 m^2/g(Kores). pore size distribution curves indicate a sharp peak at about 20-30 A for all samples. (2) Cation exchange capacity (CEC) was measured by "Equilibrium Method". CEC range from 4.83 meg/100g(Vallecas) to 1.17 meg/100g(Kuzuu) when the pH of the solution is 7. The remarkable dependance of CEC on the pH of the solution indicate that the CEC of sepiolite is mainly caused by broken donds situated at the edges of the crystal lattice.
3. Acid treatment of sepiolite Firbous silica gel was obtained by HCL treatment of spepolete. As an exmaple, the product from the Kuzuu sepiolite, from which Mg was completely removed, shows a specific surface area of 470 m^2/g, an average pore size of 33.3 A, and a pore volume of 0.51 cc/g. These characteristics, together with a peculiar fibrous form, will make this silica gel a possible target of the new utilization.

  • Research Products

    (10 results)

All Other

All Publications (10 results)

  • [Publications] T.Kiyohiro: Bull.Sci.Eng'ng.Research Lab.,Waseda Univ.NO.110. 59-64 (1985)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] 輿水仁: 石膏と石灰. NO.204. 72-79 (1986)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] T.Kiyohiro: Clay Minerals.

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] 坂本尚史: 粘土科学.

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] 大塚良平: 日本鉱業会誌.

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] T. Kiyohiro: "Electron Optical Observation of Sepiolite "Anhydride" Structure" Bull. Sci. Eng'ng. Research Lab., Wasada Univ.No.110. 59-64 (1985)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] H. Koshimizu: "Ion Exchange og Clay %minerals" Gypsym and Lime. No.204. 72-79 (1986)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] T. Kiyohiro: "Dephydration Mechanism of Sepiolite." to be submitted to Clay Minerals.

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] T. Sakamoto: "Sepiolite from Leping, Jiangxi, China," to be submitted to Nendo Kagaku (Journal of the Clay Science Society of Japan).

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] R. Otsuka: "Fundamental Studies of Fibrous Clay Minerals." to be submitted to Jr. Min. Met. Inst. Japan.

    • Description
      「研究成果報告書概要(欧文)」より

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Published: 1989-03-30  

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