Enthalpy of mixing of solid solution rhomboclase – Indium-substituted rhomboclase (H3O) Fe1−xInx(SO4)2·nH2O

IF 2.2 3区 工程技术 Q3 CHEMISTRY, PHYSICAL
Franz Bärthel, Juraj Majzlan
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引用次数: 0

Abstract

Solid solution of rhomboclase [nominally (H3O) Fe(SO4)2·3H2O] with Fe-In substitution was synthesized by coprecipitation and hydrothermal treatment and investigated by chemical, X-ray diffraction, and thermodynamic analysis in this study. The solid solution is continuous over the whole stoichiometric range despite significant differences in ionic radii between Fe3+ and In3+. Enthalpy of formation of rhomboclase and enthalpies of mixing of solid solution rhomboclase – indium-substituted rhomboclase were determined by acid-solution calorimetry in 5 mol·dm−1 HCl at T = 298.15 K and p = 1 bar. The actual compositions of the studied synthetic end members are (H3O)0.798Fe(SO4)1.899·3.078H2O (rhomboclase with molecular mass of 308.8719 g·mol−1) and (H3O)1.067In(SO4)2.034·3.017H2O (indium-substituted rhomboclase with molecular mass of 384.8377 g·mol−1). The enthalpies of mixing were obtained for a series of four indium-incorporating rhomboclase synthetic samples with molar In/(In + Fe) ratios of 0.115, 0.226, 0.537, and 0.733. The enthalpy of formation from elements in their standard state at T = 298.15 K and p = 1 bar obtained in this study by thermochemical cycle for (H3O)0.798Fe(SO4)1.899·3.078H2O is: ΔfH298.15°=-2815.2±2.8 kJ·mol−1. Mean measured enthalpies of dissolution for (H3O)0.798Fe(SO4)1.899·3.078H2O and (H3O)1.067In(SO4)2.034·3.017H2O are: ΔdissH°=14.47±0.42 kJ·mol−1 and -6.68±0.27 kJ · mol−1, respectively. Enthalpies of mixingΔmixH° have small positive values and can be fitted by a regular solid solution model with a mixing parameter W=4.26±0.32 kJ·mol−1.

固溶体菱镁矿-铟取代菱镁矿 (H3O)Fe1-In (SO4)2-nH2O 的混合焓
本研究通过共沉淀和水热处理合成了具有 Fe-In 置换的菱锰矿[名义上为 (H3O) Fe(SO4)2-3H2O]固溶体,并通过化学、X 射线衍射和热力学分析对其进行了研究。尽管 Fe3+ 和 In3+ 的离子半径存在显著差异,但固溶体在整个化学计量范围内是连续的。在 T = 298.15 K 和 p = 1 bar 条件下,在 5 mol-dm-1 HCl 溶液中用酸溶量热法测定了菱锰矿的形成焓和固溶体菱锰矿-铟取代菱锰矿的混合焓。所研究的合成最终成员的实际成分为 (H3O)0.798Fe(SO4)1.899-3.078H2O (菱镁矿,分子质量为 308.8719 g-mol-1)和 (H3O)1.067In(SO4)2.034-3.017H2O (铟取代的菱镁矿,分子质量为 384.8377 g-mol-1)。一系列四种铟/(铟+铁)摩尔比为 0.115、0.226、0.537 和 0.733 的掺杂菱镁矿合成样品的混合焓均已获得。本研究通过热化学循环得到的 (H3O)0.798Fe(SO4)1.899-3.078H2O 在 T = 298.15 K 和 p = 1 bar 条件下元素标准状态的形成焓为:ΔfH298.15°=-2815.2±2.8 kJ-mol-1。(H3O)0.798Fe(SO4)1.899-3.078H2O 和(H3O)1.067In(SO4)2.034-3.017H2O的平均测量溶解焓为:ΔfH298.15°=-2815.2±2.8 kJ-mol-1:分别为:ΔdissH°=14.47±0.42 kJ-mol-1 和 -6.68±0.27 kJ - mol-1。混合焓ΔmixH°具有较小的正值,可以用混合参数 W=4.26±0.32 kJ-mol-1 的常规固溶体模型来拟合。
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来源期刊
Journal of Chemical Thermodynamics
Journal of Chemical Thermodynamics 工程技术-热力学
CiteScore
5.60
自引率
15.40%
发文量
199
审稿时长
79 days
期刊介绍: The Journal of Chemical Thermodynamics exists primarily for dissemination of significant new knowledge in experimental equilibrium thermodynamics and transport properties of chemical systems. The defining attributes of The Journal are the quality and relevance of the papers published. The Journal publishes work relating to gases, liquids, solids, polymers, mixtures, solutions and interfaces. Studies on systems with variability, such as biological or bio-based materials, gas hydrates, among others, will also be considered provided these are well characterized and reproducible where possible. Experimental methods should be described in sufficient detail to allow critical assessment of the accuracy claimed. Authors are encouraged to provide physical or chemical interpretations of the results. Articles can contain modelling sections providing representations of data or molecular insights into the properties or transformations studied. Theoretical papers on chemical thermodynamics using molecular theory or modelling are also considered. The Journal welcomes review articles in the field of chemical thermodynamics but prospective authors should first consult one of the Editors concerning the suitability of the proposed review. Contributions of a routine nature or reporting on uncharacterised materials are not accepted.
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