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Spinel Solid Solultions in the Li-Fe-Mn-O System

机译:Li-Fe-Mn-O系统中的尖晶石固溶体

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The ranges of Li-Fe-Mn composition in which single-phase microparticulate spinel oxides are formed by heating in air were determined. The aim was to reevaluate previously published reports on binary solid solutions between LiFe_5O_8 and Li-Mn-O spinels by covering the whole possible range of (Li, Fe, Mn)_3O_4 spinels with Mn valence higher than 3. To sensitively detect possible heterogeneity of the lemental distribution or phase composition, chemical and X-ray powder diffraction analyses were used, temperature dependence of magnetic susceptibility was obtained for samples rich in Fe, and electrochemical reductive dissolution was studied by means of voltammetry of microparticles. Instead of a continuous series of solid solutions, three regions were found with different dependence of lattice parameters on elemental composition. A region of nonuniform solid solutions was found at Fe/(Fe+Mn)>0.4 and Mn valence >3.2.
机译:确定其中通过在空气中加热形成单相微粒状尖晶石氧化物的Li-Fe-Mn组成的范围。目的是通过覆盖Mn价高于3的(Li,Fe,Mn)_3O_4尖晶石的整个可能范围,重新评估先前发表的有关LiFe_5O_8和Li-Mn-O尖晶石之间的二元固溶体的报告。通过元素分布或相组成,化学和X射线粉末衍射分析,获得了富铁样品的磁化率与温度的关系,并通过微粒伏安法研究了电化学还原溶解。代替连续的一系列固溶体,发现三个区域的晶格参数对元素组成的依赖性不同。发现Fe /(Fe + Mn)> 0.4且Mn化合价> 3.2的固溶体区域不均匀。

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