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Effect of molten sodium nitrate on the decomposition pathways of hydrated magnesium hydroxycarbonate to magnesium oxide probed by in situ total scattering

机译:熔融钠硝酸盐的影响分解途径的水合镁hydroxycarbonate氧化镁的探测现场总散射

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摘要

The effect of NaNO3 and its physical state on the thermal decomposition pathways of hydrated magnesium hydroxycarbonate (hydromagnesite, HM) towards MgO was examined by in situ total scattering. Pair distribution function (PDF) analysis of these data allowed us to probe the structural evolution of pristine and NaNO3-promoted HM. A multivariate curve resolution alternating least squares (MCR-ALS) analysis identified the intermediate phases and their evolution upon the decomposition of both precursors to MgO. The total scattering results are discussed in relation with thermogravimetric measurements coupled with off-gas analysis. MgO is obtained from pristine HM (N-2, 10 degrees C min(-1)) through an amorphous magnesium carbonate intermediate (AMC), formed after the partial removal of water of crystallization from HM. The decomposition continues via a gradual release of water (due to dehydration and dehydroxylation) and, in the last step, via decarbonation, leading to crystalline MgO. The presence of molten NaNO3 alters the decomposition pathways of HM, proceeding now through AMC and crystalline MgCO3. These results demonstrate that molten NaNO3 facilitates the release of water (from both water of crystallization and through dehydroxylation) and decarbonation, and promotes the crystallization of MgCO3 and MgO in comparison to pristine HM. MgO formed from the pristine HM precursor shows a smaller average crystallite size than NaNO3-promoted HM and preserves the initial nano-plate-like morphology of HM. NaNO3-promoted HM was decomposed to MgO that is characterized by a larger average crystallite size and irregular morphology. Additionally, in situ SEM allowed visualization of the morphological evolution of HM promoted with NaNO3 at a micrometre scale.
机译:NaNO3和其物理状态的影响水化的热分解途径镁hydroxycarbonate(水菱镁矿,嗯)对采用了原位散射。这些数据让我们调查分析构造演化的原始和NaNO3-promoted嗯。分辨率交替最小二乘(MCR-ALS)分析中间阶段和识别他们进化的分解采用的先兆。讨论了与热重吗加上测量尾气分析。从原始HM (n - 10摄氏度分钟(1)通过一个非晶态镁碳酸盐中间(AMC),部分后形成的删除嗯的结晶水。分解继续通过逐步释放水(由于脱水和脱羟基)在最后一步,通过脱二氧化碳,导致水晶分别。改变了HM的分解途径,现在通过AMC和水晶氧化物。这些结果说明熔融NaNO3促进水(从水的释放结晶,通过脱羟基)、脱二氧化碳促进了结晶的氧化物和分别比较原始的嗯。前兆显示了一个更小的平均微晶大小比NaNO3-promoted HM和保存HM的初始nano-plate-like形态。NaNO3-promoted HM分解,分别是以一个更大的平均微晶大小和不规则形态。原地SEM允许可视化形态演变与NaNO3 HM提拔在微米尺度。

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