天青石:物理化学和量热研究

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
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引用次数: 0

摘要

Abstract Destinezite ( \({\{Fe}}_{{1.97}}^{{3 + }}\) Al0.02)(PO4)0.99(SO4)0.90(OH)1.20⋅5.97H2O (捷克共和国)已通过热分析、电子探针分析、X射线粉末衍射以及红外光谱、拉曼光谱和莫斯鲍尔光谱进行了研究。在一台 Setaram(法国)Calvet 微量热仪上,通过溶液量热法测定了元素 ∆fH0(298.15 K) = -4258 ± 12 kJ/mol 在硼酸铅 2PbO⋅B2O3 熔体中的形成焓。估算了其绝对熵值 S0(298.15 K) = 462.0 J/(mol K),计算了形成熵 ∆fS0(298.15 K) = -2054 J/(mol K),以及元素形成的吉布斯能 ∆fG0(298.15 K) = -3646 kJ/mol。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Destinezite: A Physicochemical and Calorimetric Study

Abstract

Destinezite ( \({\text{Fe}}_{{1.97}}^{{3 + }}\) Al0.02)(PO4)0.99(SO4)0.90(OH)1.20⋅5.97H2O (Czech Republic) has been studied by thermal and electron-microprobe analyses, X-ray powder diffraction, and by IR, Raman, and Mössbauer spectroscopy. The enthalpy of formation of destinezite \({\text{Fe}}_{2}^{{3 + }}\) (PO4)(SO4)(OH)⋅6H2O from elements ∆fH0(298.15 K) = –4258 ± 12 kJ/mol was determined by the method of solution calorimetry in lead borate 2PbO⋅B2O3 melt on a Setaram (France) Calvet microcalorimeter. The value of its absolute entropy S0(298.15 K) = 462.0 J/(mol K) was estimated, the entropy of formation ∆fS0(298.15 K) = –2054 J/(mol K), and the Gibbs energy of formation from the elements ∆fG0(298.15 K) = –3646 kJ/mol were calculated.

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来源期刊
Geochemistry International
Geochemistry International 地学-地球化学与地球物理
CiteScore
1.60
自引率
12.50%
发文量
89
审稿时长
1 months
期刊介绍: Geochemistry International is a peer reviewed journal that publishes articles on cosmochemistry; geochemistry of magmatic, metamorphic, hydrothermal, and sedimentary processes; isotope geochemistry; organic geochemistry; applied geochemistry; and chemistry of the environment. Geochemistry International provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent. The journal welcomes manuscripts from all countries in the English or Russian language.
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