Changes in Bornite (Cu5FeS4) after Heating in Air: Mossbauer Effect Study

被引:0
|
作者
Kadziolka-Gawel, M. [1 ]
Adamczyk, Z. [2 ]
机构
[1] Univ Silesia Katowice, Inst Phys, 75 Pulku Piechoty 1a, PL-41500 Chorzow, Poland
[2] Silesian Tech Univ, Inst Appl Geol, Akad 2, PL-44100 Gliwice, Poland
关键词
SPECTROSCOPY;
D O I
10.12693/APhysPolA.134.1044
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
The phase transitions and structural behaviour in natural bornite sample were investigated after heat treatment in air in a temperature range of (180 divided by 500) degrees C using high-resolution Faraday, X-ray diffraction and (5)7Fe Mossbauer spectroscopy studies. X-ray diffraction and the Mossbauer spectroscopy results show that polymorph phases can exist only at high temperatures, and at a temperature of 220 degrees C a process of decomposition of bornite structure starts. Hematite is a main Fe-bearing phase and Cu is located mainly in cooper oxides present in the sample after annealing at 500 degrees C.
引用
收藏
页码:1044 / 1047
页数:4
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