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Dive into the research topics where Takabumi Sakamoto is active.

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Featured researches published by Takabumi Sakamoto.


Analyst | 1982

Spectrophotometric determination of uranium(VI) in phosphoric acid by means of solvent extraction with mixtures of TOPO and biphenyl

Takehiro Kojima; Yasumasa Shigetomi; Hideaki Kamba; Hirobumi Iwashiro; Takabumi Sakamoto; Akira Doi

The variations in the distribution coefficients of twelve metals and uranium between nitric acid or hydrochloric acid-TOPO (trioctylphosphine oxide) systems have been studied as functions of the concentration of nitric acid, hydrochloric acid and TOPO and temperature (in the range 70–80 °C), employing biphenyl as the diluent for TOPO. The formula UO2(NO3)2-(TOPO)2 can be assigned to the complex. Uranium in a phosphoric acid solution is quantitatively extracted from 2 mol dm–3 nitric acid into molten TOPO-biphenyl at about 70 °C. The organic phase separates out as a solid on cooling and is dissolved in ethanol. The uranium in this solution is then determined spectrophotometrically with 1-(2-pyridylazo)naphth-2-ol. Beers law holds in the range 1–8 p.p.m. of uranium, and the relative standard deviation for 10 determinations was 2.1%.


Journal of the Mineralogical Society of Japan | 1990

Some problems on chemical composition analysis of clay minerals by analytical transmission electron microscope.

Kiyoshi Okada; Takabumi Sakamoto; Hisato Hayashi

Chemical compositions of kaolinite, crocidolite, chlorite, sepiolite, chrysotile, beidelite and montmorillonite were analysed by analytical transmission electron microscope (AEM) and were compared with their bulk compositions measured by wet chemical method. Most of the data by AEM using approximately 10 nm probe size showed apparently richer in SiO2 than those by wet chemical method. No significant influence by K-factors of water was recognized by the comparison of the data of kaolinite and metakaolinite, which was prepared by dehydration of kaolinite. Data by picture mode for approximately 0.2μm×0.2μm region for kaolinite showed in good agreement with ideal composition whereas data by spot mode analysed in the same region showed apparently SiO2 rich composition, and were scattered very widely among particles. This anomaly in spot mode data was considered to be due to the channeling effect and possibly to the contamination and/or damage for the specimen by the incident electron beam.


The Journal of the Japanese Association of Mineralogists,Petrologists and Economic Geologists | 1980

IRON-SEPIOLITE FROM THE SEIKAN TUNNEL, JAPAN

Takabumi Sakamoto; Shigeru Suzuki; Hidenobu Tatematsu; Ryohei Otsuka


Clay science | 2000

Artificial weathering of granite under earth surface conditions - the influence of acid rain on rocks and minerals (Part 3).

Shoichi Kobayashi; Takabumi Sakamoto


Journal of the Clay Science Society of Japan | 1974

Phase Transformations of Sepiolite under Hydrothermal Conditions

Ryohei Otsuka; Takabumi Sakamoto; Yu Hara


The Journal of the Japanese Association of Mineralogists,Petrologists and Economic Geologists | 1973

OPAL FROM HOSAKA, FUKUSHIMA PREFECTURE, JAPAN

Sadao Tsutsumi; Takabumi Sakamoto


Archive | 2008

Artificial chemical weathering of plagioclase under earth surface conditions

Yumi Baba; Shoichi Kobayashi; Takabumi Sakamoto


Journal of the Mineralogical Society of Japan | 1990

Hydrothermal treatment of okenite. Experimental studies on the genesis of stevensite (Part 5).

Takabumi Sakamoto


Journal of the Mineralogical Society of Japan | 1979

Hydrothermal treatment of pectolite

Ryohei Otsuka; Takabumi Sakamoto; Shigeru Suzuki; Shinji Shinoda; Hitoshi Koshimizu


Preprints of Annual Meeting of The Ceramic Society of Japan Preprints of Fall Meeting of The Ceramic Society of Japan 15th Fall Meeting of The Ceramic Society of Japan | 2002

Hydrothermal synthesis of clay minerals from burned sludge

Mari Ushirouchi; Takabumi Sakamoto

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Shoichi Kobayashi

Okayama University of Science

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Hidenobu Tatematsu

Railway Technical Research Institute

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Akira Doi

Okayama University of Science

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Takatsugu Mashiko

Okayama University of Science

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Kiyoshi Okada

Tokyo Institute of Technology

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Makoto Asadu

Okayama University of Science

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