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在几何受阻尖晶石 MgVO 中引入磁性离子(Cr 和 Fe)对钒位的影响:磁性和催化性能。

Implications of including a magnetic ion (Cr and Fe) at the vanadium site in a geometrically frustrated spinel MgVO: magnetic and catalytic properties.

机构信息

Materials Chemistry Group, Department of Chemistry, University of Delhi, Delhi-110007, India.

出版信息

Dalton Trans. 2019 Nov 12;48(44):16661-16670. doi: 10.1039/c9dt03468d.

Abstract

The vanadium sublattice in a geometrically frustrated MgV2O4 is substituted partially with Cr3+ and Fe3+. With a successful Rietveld refinement of the powder X-ray diffraction patterns of MgVCrO4 and MgVFeO4, Cr and Fe occupy the octahedral sites of a spinel structure. Extensive field-dependent and temperature magnetic measurements on these samples reveal exciting results. MgV2O4 remains paramagnetic till 3 K, with a small divergence at around 20 K between ZFC and FC data. MgVCrO4 exhibits antiferromagnetic behavior with a Néel temperature of 13.6 K. MgVFeO4 shows spin-glass behavior resulting from the frustration with a glass transition temperature of 194 K. This sample shows a typical ferromagnetic behavior, with a coercivity of 194.5 Oe within an applied field of ±2 kOe. All three systems have been found to have a frustration index in the range of 1-25, and the effective magnetic moment decreases in the order MgVFeO4 > MgVCrO4 > MgV2O4. While the inclusion of chromium does not alter the bandgap of MgV2O4, iron substitution increases the bandgap. The partial replacement of V3+ with Cr3+ and Fe3+ increases the catalytic ability of the system in terms of the oxidative degradation of methylene blue dye. The catalytic efficiency follows the order MgVFeO4 > MgVCrO4 > MgV2O4, matching well with the trend noticed in the porosity, surface area, and redox ability of Fe3+, Cr3+ and V3+ in these samples. The degradation pathway has been followed by analyzing the intermediates from these experiments by mass spectrometry, and a plausible mechanism is proposed.

摘要

在几何阻挫的 MgV2O4 中,部分钒亚晶格被 Cr3+和 Fe3+取代。通过对 MgVCrO4 和 MgVFeO4 的粉末 X 射线衍射图谱进行成功的 Rietveld 精修,Cr 和 Fe 占据尖晶石结构的八面体位置。对这些样品进行广泛的场依赖和温度磁测量,揭示了令人兴奋的结果。MgV2O4 直到 3 K 仍保持顺磁性,在 ZFC 和 FC 数据之间在 20 K 左右略有发散。MgVCrO4 表现出反铁磁行为,尼尔温度为 13.6 K。MgVFeO4 由于受阻而表现出自旋玻璃行为,玻璃转变温度为 194 K。该样品表现出典型的铁磁行为,在 ±2 kOe 的外加磁场中具有 194.5 Oe 的矫顽力。所有三个系统都被发现具有 1-25 范围内的阻挫指数,有效磁矩按 MgVFeO4>MgVCrO4>MgV2O4 的顺序减小。虽然铬的加入不会改变 MgV2O4 的带隙,但铁的取代会增加带隙。V3+的部分取代为 Cr3+和 Fe3+增加了系统在氧化降解亚甲基蓝染料方面的催化能力。催化效率遵循 MgVFeO4>MgVCrO4>MgV2O4 的顺序,与这些样品中 Fe3+、Cr3+和 V3+的孔隙率、比表面积和氧化还原能力所注意到的趋势非常吻合。通过分析这些实验中的中间体的质谱,已经跟踪了降解途径,并提出了一个合理的机制。

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