Yu. D. Gritsenko, L. P. Ogorodova, M. F. Vigasina, L. V. Melchakova, D. A. Ksenofontov, S. K. Dedushenko
{"title":"天青石:物理化学和量热研究","authors":"Yu. D. Gritsenko, L. P. Ogorodova, M. F. Vigasina, L. V. Melchakova, D. A. Ksenofontov, S. K. Dedushenko","doi":"10.1134/S0016702924030042","DOIUrl":null,"url":null,"abstract":"<p>Destinezite (<span>\\({\\text{Fe}}_{{1.97}}^{{3 + }}\\)</span>Al<sub>0.02</sub>)(PO<sub>4</sub>)<sub>0.99</sub>(SO<sub>4</sub>)<sub>0.90</sub>(OH)<sub>1.20</sub>⋅5.97H<sub>2</sub>O (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 <span>\\({\\text{Fe}}_{2}^{{3 + }}\\)</span>(PO<sub>4</sub>)(SO<sub>4</sub>)(OH)⋅6H<sub>2</sub>O from elements ∆<sub>f</sub><i>H</i><sup>0</sup>(298.15 K) = –4258 ± 12 kJ/mol was determined by the method of solution calorimetry in lead borate 2PbO⋅B<sub>2</sub>O<sub>3</sub> melt on a Setaram (France) Calvet microcalorimeter. The value of its absolute entropy <i>S</i><sup>0</sup>(298.15 K) = 462.0 J/(mol K) was estimated, the entropy of formation ∆<sub>f</sub><i>S</i><sup>0</sup>(298.15 K) = –2054 J/(mol K), and the Gibbs energy of formation from the elements ∆<sub>f</sub><i>G</i><sup>0</sup>(298.15 K) = –3646 kJ/mol were calculated.</p>","PeriodicalId":12781,"journal":{"name":"Geochemistry International","volume":"62 3","pages":"274 - 283"},"PeriodicalIF":0.7000,"publicationDate":"2024-04-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Destinezite: A Physicochemical and Calorimetric Study\",\"authors\":\"Yu. D. Gritsenko, L. P. Ogorodova, M. F. Vigasina, L. V. Melchakova, D. A. Ksenofontov, S. K. Dedushenko\",\"doi\":\"10.1134/S0016702924030042\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Destinezite (<span>\\\\({\\\\text{Fe}}_{{1.97}}^{{3 + }}\\\\)</span>Al<sub>0.02</sub>)(PO<sub>4</sub>)<sub>0.99</sub>(SO<sub>4</sub>)<sub>0.90</sub>(OH)<sub>1.20</sub>⋅5.97H<sub>2</sub>O (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 <span>\\\\({\\\\text{Fe}}_{2}^{{3 + }}\\\\)</span>(PO<sub>4</sub>)(SO<sub>4</sub>)(OH)⋅6H<sub>2</sub>O from elements ∆<sub>f</sub><i>H</i><sup>0</sup>(298.15 K) = –4258 ± 12 kJ/mol was determined by the method of solution calorimetry in lead borate 2PbO⋅B<sub>2</sub>O<sub>3</sub> melt on a Setaram (France) Calvet microcalorimeter. The value of its absolute entropy <i>S</i><sup>0</sup>(298.15 K) = 462.0 J/(mol K) was estimated, the entropy of formation ∆<sub>f</sub><i>S</i><sup>0</sup>(298.15 K) = –2054 J/(mol K), and the Gibbs energy of formation from the elements ∆<sub>f</sub><i>G</i><sup>0</sup>(298.15 K) = –3646 kJ/mol were calculated.</p>\",\"PeriodicalId\":12781,\"journal\":{\"name\":\"Geochemistry International\",\"volume\":\"62 3\",\"pages\":\"274 - 283\"},\"PeriodicalIF\":0.7000,\"publicationDate\":\"2024-04-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geochemistry International\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1134/S0016702924030042\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochemistry International","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1134/S0016702924030042","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Destinezite: A Physicochemical and Calorimetric Study
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.
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.