FORMATION OF MICA DURING EXPERIMENTAL ALTERATION OF K-FELDSPAR

被引:6
作者
KAWANO, M [1 ]
TOMITA, K [1 ]
机构
[1] KAGOSHIMA UNIV,FAC SCI,INST EARTH SCI,KAGOSHIMA 890,JAPAN
关键词
DISSOLUTION MECHANISM; EXPERIMENTAL ALTERATION; FIBROUS BOEHMITE; K-FELDSPAR; MICA;
D O I
10.1346/CCMN.1995.0430402
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Experimental alterations of K-feldspar in distilled-deionized water at 150 degrees, 175 degrees, 200 degrees and 225 degrees C were performed. The alteration products and dissolution mechanism of K-feldspar were examined by X-ray powder diffraction (XRD), scanning electron microscopy (SEM), transmission electron microscopy (TEM), energy dispersive X-ray analysis (EDX), and X-ray photoelectron spectroscopy (XPS). SEM, TEM, and EDX clearly showed formation of fibrous boehmite less than 1.0 mu m in length at the early alteration stages. The boehmite fibers decreased in abundance and rounded platy 1 M mica was produced as alteration proceeded. The mica exhibited initially angular shaped small flakes of 0.69 mu m in average size, which developed to rounded platy particles of 1.97 mu m. The main chemical reactions occurring in this experimental system can be expressed by: [GRAPHICS] XPS showed no significant changes in intensities of photoelectron lines excited from K, Si, and Al in the K-feldspar surface before and after alteration, however the K/Si molar ratios in the solutions were considerably smaller than that of the original K-feldspar. The results of XPS strongly indicate that no dealkalized layer was produced on the surface, and that dissolution of K-feldspar in aqueous solution proceeded congruently by a surface-reaction mechanism. The discrepancy of mass balance in the solutions may be mainly caused by adsorption of K on the surface of boehmite.
引用
收藏
页码:397 / 405
页数:9
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