NaF-H2O 体系流体不溶区的罗曼蒂克溶解度(800°C,200 兆帕

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geochemistry International Pub Date : 2024-05-09 DOI:10.1134/S0016702923700155
A. F. Redkin, N. P. Kotova, Yu. B. Shapovalov, A. N. Nekrasov
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引用次数: 0

摘要

摘要-在很宽的氟化钠浓度范围内(从 0 到 25 wt % NaF),获得了罗曼蒂克石 (CaNa)Sb2O6F 在 P-Q 型 NaF-H2O 体系中溶解度的新数据。在 NaF 浓度为 1 至 8 mol kg-1 H2O(25 wt % NaF)的范围内,锑与罗美石和萤石的平衡浓度为 0.02-0.2 mol kg-1 H2O。根据这些数据,在 800°C、200 MPa 和 fO2 = 50 Pa 条件下,NaF-H2O 体系的流体不相溶区域(Cu2O-CuO 缓冲区)内,L1 和 L2 相中的锑浓度分别为 0.4 和 2.1 wt % Sb。我们的实验首次制备出骨架状萤石晶体和金属间化合物 Pt5Sb,它属于六方晶系,晶格参数(LP)如下:a = b = 4.56(4) Å,c = 4.229(2) Å,α = β = 90°,γ = 120°。在 800°C、Р = 200 MPa 和 fO2 ≤ 10-3.47 Pa(Cu-Cu2O 缓冲溶液)条件下,在罗曼蒂克石的不协调溶解实验中,铂囊内表面形成了五铂锑化物,导致溶液中锑浓度急剧下降(超过 1000 倍)。
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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.

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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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