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稠密液态二氧化碳的稳定性。

Stability of dense liquid carbon dioxide.

机构信息

Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.

出版信息

Proc Natl Acad Sci U S A. 2012 Sep 11;109(37):14808-12. doi: 10.1073/pnas.1120243109. Epub 2012 Aug 20.

Abstract

We present ab initio calculations of the phase diagram of liquid CO(2) and its melting curve over a wide range of pressure and temperature conditions, including those relevant to the Earth. Several distinct liquid phases are predicted up to 200 GPa and 10,000 K based on their structural and electronic characteristics. We provide evidence for a first-order liquid-liquid phase transition with a critical point near 48 GPa and 3,200 K that intersects the mantle geotherm; a liquid-liquid-solid triple point is predicted near 45 GPa and 1,850 K. Unlike known first-order transitions between thermodynamically stable liquids, the coexistence of molecular and polymeric CO(2) phases predicted here is not accompanied by metallization. The absence of an electrical anomaly would be unique among known liquid-liquid transitions. Furthermore, the previously suggested phase separation of CO(2) into its constituent elements at lower mantle conditions is examined by evaluating their Gibbs free energies. We find that liquid CO(2) does not decompose into carbon and oxygen up to at least 200 GPa and 10,000 K.

摘要

我们提出了从头算的方法来计算液态 CO2 的相图及其在很宽的压力和温度范围内的熔化曲线,包括与地球相关的条件。根据其结构和电子特性,我们预测在高达 200 GPa 和 10000 K 的条件下存在几个不同的液态相。我们提供了证据表明存在一级液-液相变,临界点位于约 48 GPa 和 3200 K,与地幔地热梯度相交;在约 45 GPa 和 1850 K 附近预测到液-液-固三相点。与已知的热力学稳定液体之间的一级相变不同,这里预测的分子和聚合态 CO2 相共存不会伴随着金属化。在已知的液-液转变中,这种没有电异常的情况是独特的。此外,我们通过评估其吉布斯自由能来检验先前提出的在更低地幔条件下 CO2 分离成其组成元素的相分离。我们发现,液态 CO2 不会在至少 200 GPa 和 10000 K 的条件下分解为碳和氧。

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Phys Rev Lett. 2009 Jan 9;102(1):015701. doi: 10.1103/PhysRevLett.102.015701. Epub 2009 Jan 5.
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Mixed threefold and fourfold carbon coordination in compressed CO2.压缩二氧化碳中的混合三重和四重碳配位
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Six-fold coordinated carbon dioxide VI.六配位二氧化碳VI
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Amorphous silica-like carbon dioxide.无定形二氧化硅类二氧化碳。
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