X-Ray Study of Behaviors of Sesquioxides Depositing in a Chromite Grain

Eiji Anbo
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Abstract

It is well known that sesquioxides, Cr2O3, Al2O3 and Fe2O3, are liberated from chromite ore by heat treatment in air. But behaviors of the sesquioxides in ores fired at temperatures below 1000°C have not been studied systematically.In this report, influences of behaviors of the sesquioxides on lattice spacing of the chromite fired below 1300°C and diffusion phenomena of the sesquioxides in the fired chromite grain were examined by X-ray diffraction and fluorescent X-ray analysis. The followings were observed (1) The lattice spacing (440) of the chromite decreased with elevation of heating temperature up to 700°-900°C in air and increased over these temperatures. The diffracted line (440) was most broadened at 700°-900°C. The X-ray pattern of the sesquioxides in α-type appeared over 700°C, and the relative intensity of the diffracted line (014) increased with decrease of its lattice spacing (014) between 700° and 1300°C. (2) By fluorescent X-ray analysis of the chromite grain, ratio of Fe2O3/Cr2O3 on the surface of the grain fired was determined. The ratio increased in the temperature range between 700° and 1100°C, and over this range decreased. So diffusion of the liberated sesguioxides in the spinel phase which presumably consists of a single crystal, was ascertamed.It was concluded that by the liberation of the sesquioxides the chromite phase was made unstable at the heating temperature of 700°-900°C, but was brought into a stable state over 700°-900°C by isolation of two different crystal phases of the sesquioxides and the spinel, with formation of a solid solution of the sesquioxides. The degree of crystallization of the two different phases was raised by heating over 700°-900°C.The author considers that the behaviors, as described above, of the sesquioxide deposited on the surface of the chromite crysta will give a valuable explanation of reactions with the chromite grain.
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铁铁矿中倍半氧化物沉积行为的x射线研究
众所周知,从铬铁矿中通过空气热处理可以释放出倍半氧化物Cr2O3、Al2O3和Fe2O3。但在低于1000℃的温度下,对倍半氧化物在矿石中的行为还没有系统的研究。本文通过x射线衍射和荧光x射线分析,研究了倍半氧化物的行为对1300℃以下焙烧铬铁矿晶格间距的影响,以及倍半氧化物在焙烧铬铁矿颗粒中的扩散现象。结果表明:(1)在空气中加热温度为700℃~ 900℃时,铬铁矿的晶格间距(440)随着温度的升高而减小,在此温度范围内晶格间距增大。衍射线(440)在700°-900°C时展宽最大。α型倍半氧化物在700°C以上出现x射线衍射,在700°~ 1300°C之间,衍射线(014)的相对强度随着晶格间距(014)的减小而增大。(2)通过对铬铁矿晶粒的荧光x射线分析,确定了焙烧晶粒表面Fe2O3/Cr2O3的比例。该比值在700 ~ 1100℃范围内增大,在此范围内减小。因此,释放的半氧化物在尖晶石相(可能由单晶组成)中的扩散被确定。结果表明,在700°-900°C的加热温度下,半氧化物的分离使铬铁矿相变得不稳定,但在700°-900°C的加热温度下,通过分离半氧化物和尖晶石的两种不同晶相,形成半氧化物的固溶体,使铬铁矿相处于稳定状态。在700°-900°C以上加热,提高了两种不同相的结晶程度。作者认为,如上所述,沉积在铬铁矿晶体表面的倍半氧化物的行为将对与铬铁矿颗粒的反应提供有价值的解释。
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