Yu Svena, Bond Toby, Rahemtulla Al, Leontowich Adam F G, Thompson Daphne, Dahn J R
Department of Chemical Engineering, Dalhousie University, Halifax, Nova Scotia, B3H 4R2, Canada.
Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia, B3H 4R2, Canada.
Small Methods. 2025 Jun 25:e2500632. doi: 10.1002/smtd.202500632.
In-situ synthesis X-ray diffraction is conducted at the Canadian Light Source to probe phase changes during the all-dry synthesis of LiNiMnCoO (NMC631) and LiNiMnO (NM73) made using either LiOH·HO or LiCO. All materials are heated up to 950 °C and held for one hour at 950 °C under flowing oxygen. The pathway to a layered phase is similar for all samples. First, a lithiated manganese oxide phase is formed at low temperature, then cations are incorporated into a rock salt phase from ≈420 °C. A spinel intermediary phase is formed before cation ordering occurs between Li and transition metal ions above 800 °C, giving rise to the intended layered hexagonal structure. Amongst the three materials tested, the layered phase of NMC631 (made using LiOH·HO) evolves at the lowest temperature of ≈820 °C and refines rapidly during the high temperature hold. The melting of LiOH coincides nicely with the oxidation of Ni, which forms the basis for the rock salt structure. It is postulated that the molten LiOH facilitates cation diffusion into the rock salt phase, allowing for an earlier formation of the layered phase in comparison to using LiCO, which has a higher decomposition temperature.
在加拿大光源处进行原位合成X射线衍射,以探测使用LiOH·H₂O或Li₂CO₃制备LiNiMnCoO(NMC631)和LiNiMnO₂(NM73)的全干法合成过程中的相变。所有材料加热至950℃,并在流动氧气下于950℃保持1小时。所有样品形成层状相的途径相似。首先,在低温下形成锂化锰氧化物相,然后在约420℃时阳离子掺入岩盐相。在高于800℃的Li和过渡金属离子之间发生阳离子有序化之前,会形成尖晶石中间相,从而产生预期的层状六方结构。在所测试的三种材料中,NMC631(使用LiOH·H₂O制备)的层状相在约820℃的最低温度下形成,并在高温保持期间迅速细化。LiOH的熔化与Ni的氧化恰好同时发生,这构成了岩盐结构的基础。据推测,与具有较高分解温度的Li₂CO₃相比,熔融的LiOH促进阳离子扩散到岩盐相中,从而允许更早地形成层状相。