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行星内部条件下冰化合物中的双超离子性。

Double superionicity in icy compounds at planetary interior conditions.

作者信息

de Villa Kyla, González-Cataldo Felipe, Militzer Burkhard

机构信息

Department of Earth and Planetary Science, University of California, Berkeley, CA, 94720, USA.

Department of Astronomy, University of California, Berkeley, CA, 94720, USA.

出版信息

Nat Commun. 2023 Nov 21;14(1):7580. doi: 10.1038/s41467-023-42958-0.

DOI:10.1038/s41467-023-42958-0
PMID:37990010
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10663582/
Abstract

The elements hydrogen, carbon, nitrogen and oxygen are assumed to comprise the bulk of the interiors of the ice giant planets Uranus, Neptune, and sub-Neptune exoplanets. The details of their interior structures have remained largely unknown because it is not understood how the compounds HO, NH and CH behave and react once they have been accreted and exposed to high pressures and temperatures. Here we study thirteen H-C-N-O compounds with ab initio computer simulations and demonstrate that they assume a superionic state at elevated temperatures, in which the hydrogen ions diffuse through a stable sublattice that is provided by the larger nuclei. At yet higher temperatures, four of the thirteen compounds undergo a second transition to a novel doubly superionic state, in which the smallest of the heavy nuclei diffuse simultaneously with hydrogen ions through the remaining sublattice. Since this transition and the melting transition at yet higher temperatures are both of first order, this may introduce additional layers in the mantle of ice giant planets and alter their convective patterns.

摘要

氢、碳、氮和氧元素被认为构成了冰巨行星天王星、海王星以及海王星以下系外行星内部的大部分物质。它们内部结构的细节在很大程度上仍然未知,因为人们并不了解化合物HO、NH和CH一旦被吸积并暴露于高压和高温下会如何表现和反应。在这里,我们用从头算计算机模拟研究了13种H-C-N-O化合物,并证明它们在高温下会呈现超离子态,其中氢离子通过由较大原子核提供的稳定亚晶格扩散。在更高的温度下,这13种化合物中的四种会经历第二次转变,进入一种新型的双超离子态,其中最小的重原子核与氢离子同时通过剩余的亚晶格扩散。由于这种转变以及在更高温度下的熔化转变都是一级的,这可能会在冰巨行星的地幔中引入额外的层次,并改变它们的对流模式。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/f069b06d317f/41467_2023_42958_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/0385acb711ec/41467_2023_42958_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/da1ca186719a/41467_2023_42958_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/fb94239f6aaa/41467_2023_42958_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/f069b06d317f/41467_2023_42958_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/0385acb711ec/41467_2023_42958_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/da1ca186719a/41467_2023_42958_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/fb94239f6aaa/41467_2023_42958_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d52c/10663582/f069b06d317f/41467_2023_42958_Fig4_HTML.jpg

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本文引用的文献

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The stability of FeH and hydrogen transport at Earth's core mantle boundary.铁氢化物的稳定性与氢在地球核幔边界的传输
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Magnesium oxide-water compounds at megabar pressure and implications on planetary interiors.氧化镁-水化合物在兆巴压力下的性质及其对行星内部的影响。
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Direct H-He chemical association in superionic FeOHHe at deep-Earth conditions.在地球深部条件下超离子态FeOHHe中的直接H-He化学缔合
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Evidence and Stability Field of fcc Superionic Water Ice Using Static Compression.利用静态压缩研究面心立方结构超离子态水冰的证据与稳定性场
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Superionic Silica-Water and Silica-Hydrogen Compounds in the Deep Interiors of Uranus and Neptune.天王星和海王星深层内部的超离子二氧化硅 - 水和二氧化硅 - 氢化合物。
Phys Rev Lett. 2022 Jan 21;128(3):035702. doi: 10.1103/PhysRevLett.128.035702.
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Ultrahigh-Pressure Magnesium Hydrosilicates as Reservoirs of Water in Early Earth.超高压镁水硅酸盐作为早期地球的水源
Phys Rev Lett. 2022 Jan 21;128(3):035703. doi: 10.1103/PhysRevLett.128.035703.
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Dynamic compression of water to conditions in ice giant interiors.水向冰巨行星内部条件的动态压缩。
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