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Synthesis and characterization of the LDH hydrotalcite-pyroaurite solid-solution series

机译:LDH水滑石-黄铁矿固溶体系列的合成与表征

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A layered double hydroxide (LDH) hydrotalcite-pyroaurite solid-solution series Mg_3(Al_xFe_(1-x))(CO_3)_(0.5)(OH)_8 with 1-x=0.0, 0.1……1.0 was prepared by co-precipitation at 23 ± 2℃ and pH = 1.40 ±0.03. The compositions of the solids and the reaction solutions were determined using ICP-OES (Mg, Al, Fe, and Na) and TGA techniques (CO_3~(2-), OH~-, and H_2O). Powder X-ray difraction was employed for phase identification and determination of the unit cell parameters ao and co from peak profile analysis. The parameter a_0= b_0 was found to be a linear function of the composition. This dependency confirms Vegard's law and indicates the presence of a continuous solid-solution series in the hydrotalcite-pyroaurite system. TGA data show that the temperatures at which interlayer H_2O molecules and CO_3~(2-)anions are lost, and at which dehydroxylation of the layers occurs, all decrease with increasing mole fraction of iron within the hydroxide layers. Features of the Raman spectra also depend on the iron content. The absence of Raman bands for Fe-rich members (x_(Fe)> 0.5) is attributed to possible fluorescence phenomena. Based on chemical analysis of both the solids and the reaction solutions after synthesis, preliminary Gibbs free energies of formation have been estimated. Values of ΔG°_f(hydrotalcite) = - 3773.3 ± 51.4 kJ/mol and ΔG°_f(pyroaurite) = - 3294.5 ± 95.8 kJ/mol were found at 296.15 K. The formal uncertainties of these formations constants are very high. Derivation of more precise values would require carefully designed solubility experiments and improved analytical techniques.
机译:层状双氢氧化物(LDH)水滑石-黄铁矿固溶体系列Mg_3(Al_xFe_(1-x))(CO_3)_(0.5)(OH)_8 1-x = 0.0,0.1……1.0在23±2℃和pH = 1.40±0.03时沉淀。使用ICP-OES(镁,铝,铁和钠)和TGA技术(CO_3〜(2-),OH〜和H_2O)确定固体和反应溶液的组成。粉末X射线衍射用于鉴定相和从峰轮廓分析确定晶胞参数ao和co。发现参数a_0 = b_0是成分的线性函数。这种依赖性证实了维加德定律,并表明在水滑石-黄铁矿体系中存在连续的固溶体系列。 TGA数据表明,层间H_2O分子和CO_3〜(2-)阴离子消失以及层发生脱羟基的温度都随着氢氧化物层中铁的摩尔分数的增加而降低。拉曼光谱的特征还取决于铁含量。富铁成员(x_(Fe)> 0.5)不存在拉曼谱带是由于可能的荧光现象。基于固体和合成后反应溶液的化学分析,已初步估计了吉布斯形成的自由能。在296.15 K处发现ΔG°_f(水滑石)=-3773.3±51.4 kJ / mol和ΔG°_f(黄铁矿)=-3294.5±95.8 kJ / mol的值。这些地层常数的形式不确定性非常高。推导更精确的值将需要精心设计的溶解度实验和改进的分析技术。

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