A. F. Redkin, N. P. Kotova, Yu. B. Shapovalov, A. N. Nekrasov
{"title":"NaF-H2O 体系流体不溶区的罗曼蒂克溶解度(800°C,200 兆帕","authors":"A. F. Redkin, N. P. Kotova, Yu. B. Shapovalov, A. N. Nekrasov","doi":"10.1134/S0016702923700155","DOIUrl":null,"url":null,"abstract":"<p>New data on roméite (CaNa)Sb<sub>2</sub>O<sub>6</sub>F solubility in the NaF–H<sub>2</sub>O system of P–Q type have been obtained within a wide range of sodium fluoride concentrations (from 0 to 25 wt % NaF). The concentration of antimony, in equilibrium with roméite and fluorite, in the range of NaF concentrations from 1 to 8 mol kg<sup>–1</sup> H<sub>2</sub>O (25 wt % NaF), is in the range of 0.02–0.2 mol kg<sup>–1</sup> H<sub>2</sub>O. According to the data, the concentration of antimony in phases <i>L</i><sub>1</sub> and <i>L</i><sub>2</sub> in the region of fluid immiscibility of the NaF–H<sub>2</sub>O system at 800°C, 200 MPa and <i>f</i>O<sub>2</sub> = 50 Pa, specified by the Cu<sub>2</sub>O–CuO buffer, is 0.4 and 2.1 wt % Sb, respectively. Our experiments were the first ever to produce skeletal fluorite crystals and the intermetallic compound Pt<sub>5</sub>Sb, which belongs the hexagonal crystal system and has the following lattice parameters (LP): <i>a</i> = <i>b</i> = 4.56(4) Å, <i>c</i> = 4.229(2) Å, and α = β = 90°, γ = 120°. Pentaplatinum antimonide was formed on the inner surface of the Pt capsules at 800°C, <i>Р</i> = 200 MPa, and <i>f</i>O<sub>2</sub> ≤ 10<sup>–3.47</sup> Pa (Cu–Cu<sub>2</sub>O buffer) in experiments on the incongruent dissolution of roméite, which causes a sharp decrease (more than 1000 times) in antimony concentration in the solution.</p>","PeriodicalId":12781,"journal":{"name":"Geochemistry International","volume":"62 4","pages":"384 - 392"},"PeriodicalIF":0.7000,"publicationDate":"2024-05-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Roméite Solubility in the Fluid Immiscibility Region of the NaF–H2O System at 800°C, 200 MPa\",\"authors\":\"A. F. Redkin, N. P. Kotova, Yu. B. Shapovalov, A. N. Nekrasov\",\"doi\":\"10.1134/S0016702923700155\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>New data on roméite (CaNa)Sb<sub>2</sub>O<sub>6</sub>F solubility in the NaF–H<sub>2</sub>O system of P–Q type have been obtained within a wide range of sodium fluoride concentrations (from 0 to 25 wt % NaF). The concentration of antimony, in equilibrium with roméite and fluorite, in the range of NaF concentrations from 1 to 8 mol kg<sup>–1</sup> H<sub>2</sub>O (25 wt % NaF), is in the range of 0.02–0.2 mol kg<sup>–1</sup> H<sub>2</sub>O. According to the data, the concentration of antimony in phases <i>L</i><sub>1</sub> and <i>L</i><sub>2</sub> in the region of fluid immiscibility of the NaF–H<sub>2</sub>O system at 800°C, 200 MPa and <i>f</i>O<sub>2</sub> = 50 Pa, specified by the Cu<sub>2</sub>O–CuO buffer, is 0.4 and 2.1 wt % Sb, respectively. Our experiments were the first ever to produce skeletal fluorite crystals and the intermetallic compound Pt<sub>5</sub>Sb, which belongs the hexagonal crystal system and has the following lattice parameters (LP): <i>a</i> = <i>b</i> = 4.56(4) Å, <i>c</i> = 4.229(2) Å, and α = β = 90°, γ = 120°. Pentaplatinum antimonide was formed on the inner surface of the Pt capsules at 800°C, <i>Р</i> = 200 MPa, and <i>f</i>O<sub>2</sub> ≤ 10<sup>–3.47</sup> Pa (Cu–Cu<sub>2</sub>O buffer) in experiments on the incongruent dissolution of roméite, which causes a sharp decrease (more than 1000 times) in antimony concentration in the solution.</p>\",\"PeriodicalId\":12781,\"journal\":{\"name\":\"Geochemistry International\",\"volume\":\"62 4\",\"pages\":\"384 - 392\"},\"PeriodicalIF\":0.7000,\"publicationDate\":\"2024-05-09\",\"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/S0016702923700155\",\"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/S0016702923700155","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}
Roméite Solubility in the Fluid Immiscibility Region of the NaF–H2O System at 800°C, 200 MPa
New data on roméite (CaNa)Sb2O6F solubility in the NaF–H2O system of P–Q type have been obtained within a wide range of sodium fluoride concentrations (from 0 to 25 wt % NaF). The concentration of antimony, in equilibrium with roméite and fluorite, in the range of NaF concentrations from 1 to 8 mol kg–1 H2O (25 wt % NaF), is in the range of 0.02–0.2 mol kg–1 H2O. According to the data, the concentration of antimony in phases L1 and L2 in the region of fluid immiscibility of the NaF–H2O system at 800°C, 200 MPa and fO2 = 50 Pa, specified by the Cu2O–CuO buffer, is 0.4 and 2.1 wt % Sb, respectively. Our experiments were the first ever to produce skeletal fluorite crystals and the intermetallic compound Pt5Sb, which belongs the hexagonal crystal system and has the following lattice parameters (LP): a = b = 4.56(4) Å, c = 4.229(2) Å, and α = β = 90°, γ = 120°. Pentaplatinum antimonide was formed on the inner surface of the Pt capsules at 800°C, Р = 200 MPa, and fO2 ≤ 10–3.47 Pa (Cu–Cu2O buffer) in experiments on the incongruent dissolution of roméite, which causes a sharp decrease (more than 1000 times) in antimony concentration in the solution.
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.