DISSOLUTION KINETICS OF PHLOGOPITE UNDER ACID CONDITIONS
スポンサーリンク
概要
- 論文の詳細を見る
Dissolution kinetics of phlogopite were studied at 50, 80 and 120℃ using 20 ml and 100 ml of 0.01 N HCl solutions containing 0.1 M NaCl (pH l.9). The residual solid materials showed the formation of many etch pits and leached layers. The etch pits are formed more easily on the side surfaces than on the cleavage surfaces of phlogopite. The leached layer which was formed around of the flakes is composed of vermiculite and interstratified mica/vermiculite. These reveal that the dissolution of phlogopite crystal proceeds anisotropically and the dissolution rate is relatively greater along the a and b axis directions than along the c axis direction. The release rates of cations other than Si from phlogopite are explained by a diffusion kinetic equation based on a contracting disk model. The Si release, which is controlled by a surface reaction mechanism, is much slower than the other cations, and is a rate-limiting process of the entire dissolution of phlogopite. The dissolution rates of phlogopite depend on water/solid ratios used in this experiment, and were about six times faster in the 100 ml experiments than in the 20 ml experiments. The degree of incongruency of dissolution was also more significant in the 100 ml experiments than in the 20 ml experiments. The calculated activation energies for release of cations in the 100 ml experiments, followed the order, Si > Fe, Mg, Al > K, which could be related to the priority of release of cations from phlogopite structure. The activation energies for the cations other than Si (45-55 kJ/mol) were higher than those reported previously for a diffusion process of cations from phyllosilicates into solution (〜40 kJ/mol). This is probably due to the existence of vermiculite and interstratified mica/vermiculite which acts as a diffusion-inhibiting layer.
- 日本粘土学会の論文
- 1999-11-01
著者
-
Kuwahara Yoshihiro
Department Of Evolution Of Earth Environments Graduate School Of Social And Cultural Studies Kyushu
-
AOKI YOSHIKAZU
Department of Earth and Planetary Sciences, Faculty of Science, Kyushu University
-
Kuwahara Yoshihiro
Department Of Applied Chemistry Faculty Of Engineering Osaka University
-
Aoki Yoshikazu
Department Of Agricultural Chemistry The University Of Tokyo
-
Aoki Yoshikazu
Department Of Earth And Planetary Sciences Faculty Of Science Kyushu University
関連論文
- DISSOLUTION KINETICS OF PHLOGOPITE UNDER ACID CONDITIONS
- T Cell Response to Hen's Egg Ovomucoid(Biological Chemistry)
- Comparison of Four Distinct Idiotypes of Monoclonal Antibodies against Hen's Egg Ovomucoid(Biological Chemistry)
- Geology of the summit limestone of Mount Qomolangma (Everest) and cooling history of the Yellow Band under the Qomolangma detachment
- CHANGES IN POLYAMINE METABOLISM IN RAT LIVER AFTER ORAL ADMINISTRATION OF ALPHA-NAPHTHYLISOTHIOCYANATE
- TRANSMIGRATION OF MITOCHONDRIAL GOT IN CHOLESTATIC LIVER INJURY
- CHANGES IN POLYAMINE METABOLISM OF RAT LIVER AFTER ORAL ADMINISTRATION OF ALPHA-NAPHTHYLISOTHIOCYANATE
- Oxidation Mechanism of NAD Dimer Model Compounds
- In-situ, Real Time AFM Study of Smectite Dissolution under High pH Conditions at 25°-50℃(Physical and Chemical Properties of Clays,Proceedings of the 13^ International Clay Conference)
- COOL-STAGE AFM, A NEW AFM METHOD FOR IN SITU OBSERVATIONS OF MINERAL GROWTH AND DISSOLUTION AT REDUCED TEMPERATURE : INVESTIGATION OF THE RESPONSIVENESS AND ACCURACY OF THE COOLING SYSTEM AND A PRELIMINARY EXPERIMENT ON BARITE GROWTH
- COOL-STAGE AFM, A NEW AFM METHOD FOR IN SITU OBSERVATIONS OF MINERAL GROWTH AND DISSOLUTION AT REDUCED TEMPERATURE : INVESTIGATION OF THE RESPONSIVENESS AND ACCURACY OF THE COOLING SYSTEM AND A PRELIMINARY EXPERIMENT ON BARITE GROWTH