Preparation of aqueous sols of tungsten oxide dihydrate from sodium tungstate by an ion-exchange method

被引:62
|
作者
Choi, YG
Sakai, G
Shimanoe, K
Miura, N
Yamazoe, N
机构
[1] Kyushu Univ, Fac Engn Sci, Dept Mol & Mat Sci, Fukuoka 8168580, Japan
[2] Kyushu Univ, Interdisciplinary Grad Sch Engn Sci, Dept Mol & Mat Sci, Fukuoka 8168580, Japan
[3] Kyushu Univ, Adv Sci & Technol Ctr Cooperat Res, Fukuoka 8168580, Japan
关键词
tungsten oxide; sol; colloid suspension; ion exchange; sodium tungstate; preferred orientation;
D O I
10.1016/S0925-4005(02)00218-6
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Aqueous sols of tungsten oxide dihydrate (WO3.2H(2)O) were prepared from Na2WO4 by an ion-exchange method. An aqueous solution of Na2WO4 was let to flow through a glass column packed with protonated cation-exchange resin. The effluent, initially transparent, turned into an opaque viscous fluid (pale yellow) in a few hours, before yellow precipitate deposited to completion in three days. The precipitate was a mixture of a crystalline phase Of WO3.2H(2)O and an amorphous phase, and the crystalline part could be separated from another by washing with deionized water and centrifuging. The gel Of WO3.2H(2)O thus obtained consisted of platelike crystallite 25 nm thick and 42 nm. wide as evaluated from the X-ray diffractometer (XRD) peaks, and could be dispersed well into deionized water to form a stable suspension of colloidal particles with a mean diameter of about 30 nm. The mean particle size as well as the crystallite size tended to increase gradually with the repetition of dispersion in water under ultrasonic wave agitation and gelling by centrifuging. On heating, the gel (WO3.2H(2)O) changed to the monohydrate (WO3.H2O) at 100 degreesC, which in turn changed to the anhydride (WO3) at 240 degreesC. Remarkably XRD patterns showed conspicuous preferred orientation Of WO3.2H(2)O crystallites in (0 1 0) plane after the sol was centrifuged for a long time (10 h) and, upon dehydration, it was inherited by the dehydrated phases, resulting in the conspicuous orientation Of WO3 crystallites in (0 0 1). (C) 2002 Elsevier Science B.V. All rights reserved.
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页码:63 / 72
页数:10
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