Computational Investigation of Al2O3 Structures at Super-Earth Interior Conditions

IF 2.6 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY
ACS Earth and Space Chemistry Pub Date : 2026-09-17 Epub Date: 2026-08-21 DOI:10.1021/acsearthspacechem.6c00125
Stefano Racioppi, Amelia Kelly, Eva Zurek
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引用次数: 0

Abstract

Al2O3 is an important component of rocky planetary interiors, yet its behavior at the multimegabar pressures relevant to super-Earth mantles is not completely understood. Here, we combine crystal structure prediction with state-of-the-art density functional theory (DFT) calculations to investigate the structural, thermodynamic, and electronic properties of alumina from ambient pressure to 1 TPa and up to 8000 K. Evolutionary searches uncovered a previously unreported monoclinic P21/m polymorph that becomes nearly degenerate in enthalpy with the U2S3-type and α-Gd2S3-type structures above 500 GPa. Cold enthalpy calculations using the r2SCAN meta-GGA (meta-generalized-gradient approximation) functional predict the transition sequence α-Al2O3 → Rh2O3(II)-type → CaIrO3-type → U2S3-type, with the CaIrO3- to U2S3-type transition occurring at ∼450 GPa, significantly higher than earlier local-density approximation (LDA) estimates, suggesting that the U2S3-type phase may be accessible primarily under dynamic compression conditions. Quasi-harmonic free energy calculations further indicate that this transition pressure is temperature dependent up to 8000 K, with a positive slope of 94.1 K/GPa (or 10.6 MPa/K) for the phase boundary of the CaIrO3-type/U2S3-type structures. Across the stable phases, we analyze the trends of the atomic volumes, Bader charges, and electronic band gaps, revealing limited compressibility of Al3+ above 200 GPa. The predicted small enthalpy differences among high-pressure polymorphs imply the possible coexistence of numerous metastable structures under super-Earth interior conditions. These results refine the phase diagram of Al2O3 at extreme conditions and provide quantitative constraints for modeling the mineralogy, density profiles, and transport properties of rocky exoplanet mantles. We further predict that alumina remains a wide-band gap insulator throughout the investigated pressure range, with phase-dependent discontinuities of the band gap at structural transitions, but no indication of metallization up to 1 TPa and 0 K.

超地球内部条件下Al2O3结构的计算研究
Al2O3是岩石行星内部的重要组成部分,但它在与超级地球地幔相关的兆巴压力下的行为尚未完全了解。在这里,我们将晶体结构预测与最先进的密度泛函理论(DFT)计算相结合,研究氧化铝在环境压力到1tpa和高达8000k时的结构、热力学和电子特性。进化搜索发现了一种以前未报道的单斜P21/m多晶,在500 GPa以上的u2s3型和α- gd2s3型结构中,其焓几乎为简并。使用r2SCAN meta-GGA (meta-广义梯度近似)泛函计算冷焓,预测α-Al2O3→Rh2O3(II)型→CaIrO3→u2s3型转变顺序,其中CaIrO3-向u2s3型转变发生在~ 450 GPa,显著高于先前的局部密度近似(LDA)估计,表明u2s3型相可能主要在动态压缩条件下可获得。准谐波自由能计算进一步表明,在8000K以下,该转变压力与温度有关,且在cairo3型/ u2s3型结构相界处的正斜率为94.1 K/GPa(或10.6 MPa/K)。在稳定相中,我们分析了Al3+的原子体积、Bader电荷和电子带隙的变化趋势,揭示了Al3+在200gpa以上的有限压缩性。预测的高压多晶之间的小焓差意味着在超地球内部条件下可能存在许多亚稳结构。这些结果完善了极端条件下Al2O3的相图,并为岩石系外行星地幔的矿物学、密度剖面和输运特性建模提供了定量约束。我们进一步预测,在整个研究的压力范围内,铝仍然是一个宽带隙绝缘体,在结构转变时,带隙的相位依赖不连续,但在1 TPa和0K时没有金属化的迹象。
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来源期刊
ACS Earth and Space Chemistry
ACS Earth and Space Chemistry Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
5.30
自引率
11.80%
发文量
249
期刊介绍: The scope of ACS Earth and Space Chemistry includes the application of analytical, experimental and theoretical chemistry to investigate research questions relevant to the Earth and Space. The journal encompasses the highly interdisciplinary nature of research in this area, while emphasizing chemistry and chemical research tools as the unifying theme. The journal publishes broadly in the domains of high- and low-temperature geochemistry, atmospheric chemistry, marine chemistry, planetary chemistry, astrochemistry, and analytical geochemistry. ACS Earth and Space Chemistry publishes Articles, Letters, Reviews, and Features to provide flexible formats to readily communicate all aspects of research in these fields.
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