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Capturing Phase Evolution during Solvothermal Synthesis of Metastable Cu4O3

机译:溶剂热合成亚稳Cu4O3期间捕获相演化

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摘要

The metastability of Cu4O3 has long hindered the synthetic preparation of bulk samples with substantial crystallinity. The lack of suitable samples has thwarted the detailed understanding of the magnetic properties of Cu4O3 and the ability to tune its properties. While Cu4O3 was recently shown to form in solvothermal reactions, the results are unpredictable, and the crystals are small. We developed a new, more uniform synthesis technique using sealed fused silica tubes. Interrogation of the solid and liquid phases resulting from this reaction has shed more light on the kinetic evolution of copper containing phases and the microstructural correlation between different precipitation products. We find that direct conversion of the intermediate phase Cu-2(NO3)(OH)(3) to Cu4O3 is a likely consequence of dimethylformamide (DMF) triggered in situ reduction. The optimal reduction environment should be more straightforward to attain given the improved reliability of our method, and it remains under investigation. We verify the formation of Cu4O3 via X-ray diffraction, Raman microscopy, and SQUID magnetometry.
机译:长期以来,Cu4O3的亚稳性一直阻碍了具有明显结晶度的大块样品的合成制备。缺少合适的样品阻碍了对Cu4O3磁性和调节其性能的详细了解。尽管最近发现在溶剂热反应中会形成Cu4O3,但结果是无法预测的,而且晶体很小。我们使用密封的熔融石英管开发了一种新的,更均匀的合成技术。由该反应产生的固相和液相的询问为含铜相的动力学演变以及不同沉淀产物之间的微观结构相关性提供了更多的信息。我们发现中间相Cu-2(NO3)(OH)(3)直接转化为Cu4O3是触发原位还原的二甲基甲酰胺(DMF)的可能结果。考虑到我们方法的可靠性提高,最佳还原环境应该更容易实现,并且仍在研究中。我们通过X射线衍射,拉曼显微镜和SQUID磁力计验证了Cu4O3的形成。

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