Diffusion of Eu, Ce and Lu in orthopyroxene

IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Maria A. Dias, Ralf Dohmen, Nils Hartmann
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Abstract

We have measured diffusion coefficients for Eu, Lu and Ce in single crystal orthopyroxene (opx) using thin film diffusion couples produced by pulsed laser deposition. The diffusion experiments were conducted in CO-CO2 vertical gas mixing furnaces in the temperature range of T = 950–1100 °C and fO2 = 10−7 to 10−11 Pa. The microstructure of a subset of samples was investigated by scanning transmission electron microscopy (STEM) and backscattered secondary electron microscopy (BSE) in lamellae prepared using a focused ion beam – scanning electron microscope (FIB-SEM). The results were used for the interpretation of depth profiles acquired using time of flight – secondary ion mass spectrometry. This analytical approach allowed to identify low-concentration regions of the diffusion profiles, unaffected by artefacts, that could be fit to determine diffusion coefficients of Eu, Lu, and Ce. We found faster diffusion rates for Lu, Eu and Ce than previously reported for orthopyroxene and diopside. The obtained activation energies are comparable to previous studies of Lu diffusion in diopside and Nd diffusion in opx, along the iron-wüstite buffer. Our results suggest that Lu diffusion is seemingly dependent on Lu concentration and fO2, indicating a different diffusion mechanism than for Eu and Ce. Assuming that Eu is mostly in the trivalent state, we observed a trend of decreasing diffusivity with increasing ionic radii. The experimental data defines the following Arrhenius equations for Lu, Ce and Eu:
Eu、Ce和Lu在正辉石中的扩散
利用脉冲激光沉积法制备薄膜扩散偶,测量了铕、Lu和Ce在单晶正硅石(opx)中的扩散系数。扩散实验在CO-CO2垂直气体混合炉中进行,温度范围为T = 950 ~ 1100℃,fO2 = 10−7 ~ 10−11 Pa。利用聚焦离子束扫描电镜(FIB-SEM)制备的薄片,采用扫描透射电子显微镜(STEM)和背散射二次电子显微镜(BSE)研究了部分样品的微观结构。结果用于解释利用飞行时间-二次离子质谱法获得的深度剖面。这种分析方法可以识别扩散曲线的低浓度区域,不受人工制品的影响,可以适合于确定Eu, Lu和Ce的扩散系数。我们发现Lu, Eu和Ce的扩散速率比之前报道的正辉石和透辉石更快。得到的活化能与先前研究的Lu在透辉石中的扩散和Nd在opx中的扩散相当,沿着铁- wstite缓冲。我们的研究结果表明,Lu的扩散似乎依赖于Lu浓度和fO2,表明与Eu和Ce不同的扩散机制。假设Eu大部分处于三价态,我们观察到扩散率随离子半径的增大而减小。实验数据定义了Lu、Ce和Eu的Arrhenius方程:
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta 地学-地球化学与地球物理
CiteScore
9.60
自引率
14.00%
发文量
437
审稿时长
6 months
期刊介绍: Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes: 1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids 2). Igneous and metamorphic petrology 3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth 4). Organic geochemistry 5). Isotope geochemistry 6). Meteoritics and meteorite impacts 7). Lunar science; and 8). Planetary geochemistry.
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