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DOI | 10.1016/j.epsl.2021.116849 |
High-pressure experimental constraints of partitioning behavior of Si and S at the Mercury's inner core boundary | |
Tao R.; Fei Y. | |
发表日期 | 2021 |
ISSN | 0012821X |
卷号 | 562 |
英文摘要 | The partitioning of light elements between liquid and solid at the inner core boundary (ICB) governs compositional difference and density deficit between the outer and inner core. Observations of high S and low Fe concentration on the surface of Mercury from MESSENGER mission indicate that Mercury is formed under much more reduced conditions than other terrestrial planets, which may result in a Si and S-bearing metallic Fe core. In this study, we conducted high-pressure experiments to investigate the partitioning behavior of Si and S between liquid and solid in the Fe-Si-S system at 15 and 21 GPa, relevant to Mercury's ICB conditions. Experimental results show that almost all S partitions into liquid. The partitioning coefficient of Si (DSi) between liquid and solid is strongly correlated with the S content in liquid (XSliquid) as: log10(DSi)=0.0445+5.9895⁎log10(1−XSliquid). Within our experimental range, pressure has limited effect on the partitioning behavior of Si and S between liquid and solid. For Mercury with an Fe-Si-S core, compositional difference between the inner and outer core is strongly dependent on the S content of the core. The lower S content is in the core, the smaller compositional difference and density deficit between the liquid outer core and solid inner core should be observed. For a core with 1.5 wt% bulk S, a model ICB temperature would intersect with the melting curve at ∼17 GPa, corresponding to an inner core with a radius of ∼1600 km. © 2021 Elsevier B.V. |
关键词 | Fe-Si-Shigh-pressureMercury's corepartitioningphase diagram |
英文关键词 | Iron; Iron compounds; Liquids; Compositional difference; High-pressure experiment; Inner core boundary; Light elements; Melting curves; Outer and inner cores; Partitioning coefficients; Terrestrial planets; Silicon; experimental study; high pressure; inner core; iron; Mercury (planet); partition coefficient; silicon; sulfur |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/203304 |
作者单位 | Earth and Planets Laboratory, Carnegie Institution for Science, 5251 Broad Branch Road, NW, Washington, DC 20015, United States |
推荐引用方式 GB/T 7714 | Tao R.,Fei Y.. High-pressure experimental constraints of partitioning behavior of Si and S at the Mercury's inner core boundary[J],2021,562. |
APA | Tao R.,&Fei Y..(2021).High-pressure experimental constraints of partitioning behavior of Si and S at the Mercury's inner core boundary.Earth and Planetary Science Letters,562. |
MLA | Tao R.,et al."High-pressure experimental constraints of partitioning behavior of Si and S at the Mercury's inner core boundary".Earth and Planetary Science Letters 562(2021). |
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