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首页> 外文期刊>Hyperfine Interactions >Morin transition suppression in Polycrystalline 57Hematite (α-Fe2O3) exposed to 56Fe(II)
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Morin transition suppression in Polycrystalline 57Hematite (α-Fe2O3) exposed to 56Fe(II)

机译:暴露于56 Fe(II)的多晶57 赤铁矿(α-Fe2 O3 )中的Morin跃迁抑制

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摘要

We used the isotope selectivity of 57Fe M?ssbauer spectroscopy to investigate changes in the magnetic properties of polycrystalline hematite exposed to ferrous iron (Fe(II)). We found that sorption of 56Fe(II), followed by interfacial electron exchange, alters the bulk magnetic properties of 57hematite. After reaction with 56Fe(II), we observed partial suppression of the Morin transition of 57hematite to below 13 K. This is significantly lower than the Morin temperature (T M) of ~230 K measured for isotopically enriched polycrystalline 57hematite, as well as the T M of 264 ± 2 K reported for normal polycrystalline hematite.
机译:我们使用57 Fe M?ssbauer光谱的同位素选择性研究了暴露于亚铁(Fe(II))的多晶赤铁矿的磁性。我们发现吸附56 Fe(II),然后进行界面电子交换,改变了57 赤铁矿的体磁性能。与56 Fe(II)反应后,我们观察到57 赤铁矿的Morin转变被部分抑制到13 K以下。这明显低于〜的Morin温度(TM )同位素富集的多晶57 赤铁矿测得的值为230 K,常规多晶赤铁矿的TM值为264±2K。

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