<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v2.3 20070202//EN" "journalpublishing.dtd">
<article article-type="research-article" dtd-version="2.3" xml:lang="EN" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">
<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Earth Sci.</journal-id>
<journal-title>Frontiers in Earth Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Earth Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-6463</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="publisher-id">873088</article-id>
<article-id pub-id-type="doi">10.3389/feart.2022.873088</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Earth Science</subject>
<subj-group>
<subject>Original Research</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Ab Initio Molecular&#x2013;Dynamics Study of Structural and Bonding Properties of Liquid Fe&#x2013;Light&#x2013;Element&#x2013;O Systems Under High Pressure</article-title>
<alt-title alt-title-type="left-running-head">Ohmura et al.</alt-title>
<alt-title alt-title-type="right-running-head">Liquid Fe-Light-Element-O Systems</alt-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Ohmura</surname>
<given-names>Satoshi</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="corresp" rid="c001">&#x2a;</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1511648/overview"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Shimojo</surname>
<given-names>Fuyuki</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1726965/overview"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Tsuchiya</surname>
<given-names>Taku</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/238276/overview"/>
</contrib>
</contrib-group>
<aff id="aff1">
<sup>1</sup>
<institution>Faculty of Engineering</institution>, <institution>Hiroshima Institute of Technology</institution>, <addr-line>Hiroshima</addr-line>, <country>Japan</country>
</aff>
<aff id="aff2">
<sup>2</sup>
<institution>Department of Physics</institution>, <institution>Kumamoto University</institution>, <addr-line>Kumamoto</addr-line>, <country>Japan</country>
</aff>
<aff id="aff3">
<sup>3</sup>
<institution>Geodynamics Research Center</institution>, <institution>Ehime University</institution>, <addr-line>Matsuyama</addr-line>, <country>Japan</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>
<bold>Edited by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/1407631/overview">Simone Anzellini</ext-link>, Diamond Light Source, United Kingdom</p>
</fn>
<fn fn-type="edited-by">
<p>
<bold>Reviewed by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/1678481/overview">Anatoly Belonoshko</ext-link>, Royal Institute of Technology, Sweden</p>
<p>
<ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/571083/overview">Monica Pozzo</ext-link>, University College London, United Kingdom</p>
</fn>
<corresp id="c001">&#x2a;Correspondence: Satoshi Ohmura, <email>s.ohmura.m4@cc.it&#x2013;hiroshima.ac.jp</email>
</corresp>
<fn fn-type="other">
<p>This article was submitted to Earth and Planetary Materials, a section of the journal Frontiers in Earth Science</p>
</fn>
</author-notes>
<pub-date pub-type="epub">
<day>25</day>
<month>04</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="collection">
<year>2022</year>
</pub-date>
<volume>10</volume>
<elocation-id>873088</elocation-id>
<history>
<date date-type="received">
<day>10</day>
<month>02</month>
<year>2022</year>
</date>
<date date-type="accepted">
<day>31</day>
<month>03</month>
<year>2022</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2022 Ohmura, Shimojo and Tsuchiya.</copyright-statement>
<copyright-year>2022</copyright-year>
<copyright-holder>Ohmura, Shimojo and Tsuchiya</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/">
<p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.</p>
</license>
</permissions>
<abstract>
<p>The structural and bonding properties of liquid iron&#x2013;light&#x2013;element&#x2013;oxygen ternary systems such as Fe&#x2013;H&#x2013;O, Fe&#x2013;C&#x2013;O, Fe&#x2013;Si&#x2013;O, and Fe&#x2013;S&#x2013;O under high pressure are studied by ab initio molecular dynamics simulations. H, C, O, Si, and S are the candidate light elements in the Earth&#x2019;s outer core (liquid iron is a major constituent). From our simulations, it is found that H, C, and O show &#x201c;interstitial&#x201d; type behavior while Si and S show &#x201c;substitutional&#x201d; type behavior in the liquid iron&#x2013;light&#x2013;element&#x2013;O ternary systems. For the interactions between light elements, C&#x2013;C, Si&#x2013;Si, and Si&#x2013;O show covalent&#x2013;like interactions even under high&#x2013;pressure condition. The Si&#x2013;O covalent bond causes a shift in the ionic charge of Si to more positive, which could be related to the immiscibility of liquid Fe&#x2013;Si&#x2013;O.</p>
</abstract>
<kwd-group>
<kwd>liquid&#x2013;Fe ternary system</kwd>
<kwd>high pressure</kwd>
<kwd>liquid structure</kwd>
<kwd>bonding properties</kwd>
<kwd>molecular dynamics</kwd>
<kwd>ab initio (calculations)</kwd>
</kwd-group>
</article-meta>
</front>
<body>
<sec id="s1">
<title>1 Introduction</title>
<p>Light elements (LEs) such as hydrogen, carbon, oxygen, silicon, and sulfur are expected to exist in the Earth&#x2019;s core (<xref ref-type="bibr" rid="B6">Birch, 1964</xref>; <xref ref-type="bibr" rid="B24">Poirier, 1994</xref>; <xref ref-type="bibr" rid="B17">Mcdonough, 2003</xref>) because the core density is approximately 10% smaller than that of pure iron (<xref ref-type="bibr" rid="B6">Birch, 1964</xref>; <xref ref-type="bibr" rid="B3">Anderson and Isaak, 2002</xref>). In addition to the density, LE have a strong influence on the structural and transport properties of liquid iron under high pressure. However, there are still many uncertainties regarding the influence of LE.</p>
<p>To fully understand the thermal and magnetic behavior of the Earth, information about transport properties such as electrical and thermal conductivities of the Earth&#x2019;s outer core are required. Therefore, several experimental and theoretical studies were reported on liquid Fe alloys under high pressure, such as shock wave compression experiments (<xref ref-type="bibr" rid="B13">Keeler and Royce, 1971</xref>; <xref ref-type="bibr" rid="B16">Matassov, 1977</xref>; <xref ref-type="bibr" rid="B30">Stacey and Anderson, 2001</xref>; <xref ref-type="bibr" rid="B34">Yan et al., 2002</xref>), and first&#x2013;principle calculations (<xref ref-type="bibr" rid="B8">de Koker et al., 2012</xref>; <xref ref-type="bibr" rid="B26">Pozzo et al., 2012</xref>; <xref ref-type="bibr" rid="B27">Pozzo et al., 2013</xref>; <xref ref-type="bibr" rid="B33">Wagle et al., 2018</xref>).</p>
<p>The transport properties of liquid systems are strongly related to their liquid structures. The structural properties of liquid Fe&#x2013;LE binary systems under high pressure have therefore been investigated both theoretically and experimentally. Recently, Morard <italic>et al.</italic> clarified the compression mechanism of liquid Fe&#x2013;C from X&#x2013;ray diffraction measurements and demonstrated that the compression rate for the first coordination shell was higher than that for the second and third (<xref ref-type="bibr" rid="B19">Morard et al., 2017</xref>). Theoretically, the structures of liquid Fe&#x2013;H, Fe&#x2013;C, Fe&#x2013;N, Fe&#x2013;O, Fe&#x2013;Mg, Fe&#x2013;Si, and Fe&#x2013;S under high pressure were investigated using ab initio molecular dynamics (MD) simulations (<xref ref-type="bibr" rid="B1">Alfe and Gillan, 1998</xref>; <xref ref-type="bibr" rid="B2">Alfe et al., 1999</xref>; <xref ref-type="bibr" rid="B18">Morard et al., 2014</xref>; <xref ref-type="bibr" rid="B12">Ichikawa and Tsuchiya, 2015</xref>; <xref ref-type="bibr" rid="B25">Posner and Steinle&#x2013;Neumann, 2019</xref>; <xref ref-type="bibr" rid="B22">Ohmura et al., 2020</xref>). Alfe <italic>et al.</italic> investigated the structure of liquid Fe&#x2013;S at 330&#xa0;GPa and 6000&#xa0;K and suggested that there was no tendency for S atoms to form chains (<xref ref-type="bibr" rid="B1">Alfe and Gillan, 1998</xref>). The structural properties of liquid Fe&#x2013;O under high pressure were also investigated by ab initio MD simulations (<xref ref-type="bibr" rid="B2">Alfe et al., 1999</xref>). The distance between neighboring iron and oxygen atoms was found to be significantly shorter than the Fe&#x2013;Fe and O&#x2013;O distances. Morard et al. investigated the structural properties of liquid Fe&#x2013;O, Fe&#x2013;Si, and Fe&#x2013;S under low (5&#xa0;GPa and 2500&#xa0;K) and high (330&#xa0;GPa and 6000&#xa0;K) pressure conditions using ab initio MD simulations (<xref ref-type="bibr" rid="B18">Morard et al., 2014</xref>). From the peak positions of the radial distribution functions obtained from these simulations, it was discovered that Si was incorporated in the liquid state via substitution of Fe atoms, even at 330&#xa0;GPa. Recently, Posner et al. also performed first&#x2013;principles MD simulations for liquid Fe&#x2013;X (X &#x3d; H, C, N, O, Mg, Si, S, and Ni with 4&#xa0;at%) (<xref ref-type="bibr" rid="B25">Posner and Steinle&#x2013;Neumann, 2019</xref>), investigating diffusion coefficients and structural properties. The results showed that Si and Ni are &#x201c;iron&#x2013;like&#x201d; elements while H, C, N, O, and S were &#x201c;small non&#x2013;iron&#x2013;like&#x201d; elements. However, it was suggested that the incorporation mechanism of S shifts to substitutional when the pressure increases.</p>
<p>More recently, a systematic theoretical investigation based on ab initio MD simulations for the LE&#x2013;effect on the structural properties of liquid Fe&#x2013;LE binary systems under high pressure was reported (<xref ref-type="bibr" rid="B22">Ohmura et al., 2020</xref>). The simulation clarified that H, C, and O are incorporated into liquid Fe interstitially, while Si and S are &#x201c;substitutional&#x201d; type impurities.</p>
<p>For the Fe&#x2013;Si&#x2013;O ternary system, Pozzo et al. reported the structural properties under high pressure (<xref ref-type="bibr" rid="B27">Pozzo et al., 2013</xref>). The distance between the iron and oxygen atoms in the liquid Fe&#x2013;Si&#x2013;O was clarified to be almost the same as that in the Fe&#x2013;O binary liquid, and the Fe&#x2013;Si distance was almost the same as the iron&#x2013;iron distance. It was also found that the distance between the silicon and oxygen atoms was shorter than the distance between iron and oxygen. They additionally reported the thermal and electrical conductivities of liquid Fe (<xref ref-type="bibr" rid="B26">Pozzo et al., 2012</xref>) and Fe&#x2013;Si&#x2013;O mixtures (<xref ref-type="bibr" rid="B27">Pozzo et al., 2013</xref>) obtained from density functional theory calculations with the Kubo&#x2013;Greenwood formula at outer core conditions.</p>
<p>Recently, the immiscibility of liquid Fe&#x2013;Si&#x2013;O systems under high pressure was investigated (<xref ref-type="bibr" rid="B4">Arveson et al., 2019</xref>; <xref ref-type="bibr" rid="B11">Huang et al., 2019</xref>). Arveson et al. found immiscibility between liquid Fe&#x2013;Si and Fe&#x2013;Si&#x2013;O under high pressure, using a combination of laser&#x2013;heated diamond&#x2013;anvil cell experiments and first&#x2013;principles MD simulations. The results suggested that silicon and oxygen can coexist in the Earth&#x2019;s outer core and SiO<sub>2</sub> does not crystallize at the core&#x2013;mantle boundary (<xref ref-type="bibr" rid="B4">Arveson et al., 2019</xref>). Huang et al. also suggested that SiO<sub>2</sub> crystallization is unlikely under Earth&#x2019;s core conditions from their ab initio MD simulations (<xref ref-type="bibr" rid="B11">Huang et al., 2019</xref>).</p>
<p>In addition to Fe&#x2013;Si&#x2013;O, the liquid immiscibility of Fe&#x2013;S&#x2013;O has also been discussed. Tsuno et al. suggested that liquid&#x2013;liquid immiscibility is not expected in liquid Fe&#x2013;S&#x2013;O under high pressure, such as in the outer core condition (<xref ref-type="bibr" rid="B31">Tsuno et al., 2007</xref>). In contrast, based on thermodynamic modeling, liquid immiscibility would be still possible under the outer core conditions (<xref ref-type="bibr" rid="B9">Helffrich and Kaneshima, 2004</xref>). Recently, melting experiments of liquid Fe&#x2013;S&#x2013;O were reported, and the liquid core composition system was discussed (<xref ref-type="bibr" rid="B35">Yokoo et al., 2019</xref>).</p>
<p>Several experimental and theoretical studies on the properties of liquid Fe&#x2013;LE&#x2013;O have been reported, including the immiscibility of liquid Fe&#x2013;Si&#x2013;O and Fe&#x2013;S&#x2013;O. However, the detailed local structures, including properties of atomic bond in liquid Fe&#x2013;LE&#x2013;O ternary systems, from which various properties of the liquids originate, remain unclear. In this study to fully understand the properties of liquid Fe&#x2013;LE&#x2013;oxide ternary systems, we investigate the structural and bonding properties of liquid Fe&#x2013;O with H, C, S, and Si using ab initio MD simulations. The purpose of this study is to find unique properties of liquid ternary systems under high pressure, which cannot be observed in binary systems.</p>
<sec id="s2">
<title>2 Numerical Details</title>
<p>In our ab initio MD simulations, atomic forces were obtained from the electronic states calculated by the projector&#x2013;augmented plane&#x2013;wave (PAW) method (<xref ref-type="bibr" rid="B7">Blochl, 1994</xref>; <xref ref-type="bibr" rid="B15">Kresse and Joubert, 1999</xref>) within the framework of density functional theory (DFT). In the calculations, the generalized gradient approximation formulated by Perdew, Burke, and Ernzerhof (GGA&#x2013;PBE) was used for the exchange&#x2013;correlation potential (<xref ref-type="bibr" rid="B23">Perdew et al., 1996</xref>). The cutoff energies of the plane wave were 30 and 300 Ry for the pseudo&#x2013;wavefunctions and pseudo&#x2013;charge density, respectively. These cutoff energies were the same as those used in a previous study (<xref ref-type="bibr" rid="B22">Ohmura et al., 2020</xref>). The energy functional was minimized using an iterative scheme based on the preconditioned conjugate&#x2013;gradient method (<xref ref-type="bibr" rid="B14">Kresse and Hafner, 1994</xref>; <xref ref-type="bibr" rid="B29">Shimojo et al., 2001</xref>). The gamma point was used for the k&#x2013;point sampling. As valence electrons, 3d, 4s, and 4p states of Fe, 1s state of H, 2s and 2p states of C and O, and 3s, 3p, and 3d states of Si and S were used. We used 200 atoms in a cubic supercell under periodic boundary conditions. The thermodynamic states investigated in this study were 140&#xa0;GPa and 5000&#xa0;K. Properties of liquid Fe&#x2013;LE (LE &#x3d; H, O, C, Si and S) binary systems have been previously investigated at 140&#xa0;GPa and 5000&#xa0;K using AIMD (<xref ref-type="bibr" rid="B22">Ohmura et al., 2020</xref>). To be able to compare the results of the present work with those of the binary systems, we have used the same pressure and temperature (140&#xa0;GPa and 5000&#xa0;K). Four alloy compositions were studied: Fe160H20O20 (Fe&#x2013;H&#x2013;O), Fe160C20O20 (Fe&#x2013;C&#x2013;O), Fe160Si20O20 (Fe&#x2013;Si&#x2013;O), and Fe160S20O20 (Fe&#x2013;S&#x2013;O). Since this study does not aim to clarify the properties of liquid Fe alloy under the actual outer core condition, the compositions of the four liquids in this study were also not set to reproduce the density of outer core. To obtain each liquid state, we first prepared pure liquid Fe (liquid Fe<sub>200</sub>), and 40 Fe atoms in the liquid were randomly replaced by LEs. To make the system reach a completely disordered state without the effects of the initial configuration, we carried out MD simulations for approximately 2&#xa0;ps at a temperature 10,000&#xa0;K. Then, we decreased the temperature of the systems gradually to a target temperature to 5000&#xa0;K. After these preprocessing, to determine the density of each liquid system, a constant&#x2013;pressure MD simulations was performed for 2.4&#xa0;ps. By averaging over 1.8&#xa0;ps after equilibration, we determined the densities (volumes) in each liquid. The structural properties were investigated using MD simulations in a canonical ensemble (<xref ref-type="bibr" rid="B21">Nose, 1984</xref>; <xref ref-type="bibr" rid="B10">Hoover, 1985</xref>). Using the Nose&#x2013;Hoover thermostat technique, the equations of motion were solved via an explicit reversible integrator (<xref ref-type="bibr" rid="B32">Tuckerman et al., 1992</xref>) with a time step of &#x394;t &#x3d; 1.2&#xa0;fs for all systems except the system including hydrogen, in which the time step was 0.48&#xa0;fs. The quantities of interest were obtained by averaging over approximately 4.8&#x2013;9.6 ps after an initial equilibration taking approximately 2&#xa0;ps. In all the calculations, spin polarization was not considered.</p>
</sec>
</sec>
<sec sec-type="results|discussion" id="s3">
<title>3 Results and Discussion</title>
<sec id="s3-1">
<title>Structural Properties</title>
<p>
<xref ref-type="fig" rid="F1">Figure 1</xref> shows the densities of liquid Fe&#x2013;H&#x2013;O, Fe&#x2013;C&#x2013;O, Fe&#x2013;Si&#x2013;O, and Fe&#x2013;S&#x2013;O at 140&#xa0;GPa and 5000&#xa0;K obtained from the simulations. The densities of liquid Fe and Fe160O40 (Fe&#x2013;O) at the same P,T are also shown as solid and dashed lines, respectively. The densities of all ternary liquids are smaller than that of liquid Fe. However, in comparison with liquid Fe&#x2013;O, the densities of liquid Fe&#x2013;H&#x2013;O and Fe&#x2013;C&#x2013;O are larger than that of liquid Fe&#x2013;O, while the densities of liquid Fe&#x2013;Si&#x2013;O and Fe&#x2013;S&#x2013;O are smaller than that of liquid Fe&#x2013;O. At a lower temperature condition (<italic>T</italic> &#x3d; 3700&#xa0;K), the same behaviors can be observed (<xref ref-type="sec" rid="s9">Supplementary Figure S1</xref>).</p>
<fig id="F1" position="float">
<label>FIGURE 1</label>
<caption>
<p>Densities of liquid Fe<sub>160</sub>H<sub>20</sub>O<sub>20</sub> (Fe&#x2013;H&#x2013;O), Fe<sub>160</sub>C<sub>20</sub>O<sub>20</sub> (Fe&#x2013;C&#x2013;O), Fe<sub>160</sub>Si<sub>20</sub>O<sub>20</sub> (Fe&#x2013;Si&#x2013;O), and Fe<sub>160</sub>S<sub>20</sub>O<sub>20</sub> (Fe&#x2013;S&#x2013;O) at 140&#xa0;GPa and 5000&#xa0;K. Densities of liquid Fe and Fe<sub>160</sub>O<sub>40</sub> (Fe&#x2013;O) at 140&#xa0;GPa and 5000&#xa0;K are also displayed as solid and dashed lines, respectively.</p>
</caption>
<graphic xlink:href="feart-10-873088-g001.tif"/>
</fig>
<p>The partial pair distribution functions g&#x3b1;&#x3b2;(r) for liquid Fe&#x2013;H&#x2013;O (A), Fe&#x2013;C&#x2013;O (B), Fe&#x2013;Si&#x2013;O (C), and Fe&#x2013;S&#x2013;O (D) are shown in <xref ref-type="fig" rid="F2">Figure 2</xref>. The <italic>g</italic>
<sub>Fe&#x2013;Fe</sub>(<italic>r</italic>) has the first peak at approximately 2.2&#xa0;&#xc5; and the second peak at approximately 4&#xa0;&#xc5; in all the liquid systems. For <italic>g</italic>
<sub>O&#x2013;O</sub>(<italic>r</italic>), the profile is almost the same in each liquid, in which we can see the first peak at approximately 2.2&#xa0;&#xc5; and a small second peak at approximately 3.5&#xa0;&#xc5;. For the interactions between Fe and light elements, the first peak positions of Fe&#x2013;H, Fe&#x2013;C, and Fe&#x2013;O are smaller than that of Fe&#x2013;Fe, and the first peak positions of Fe&#x2013;Si and Fe&#x2013;S are almost the same as that of Fe&#x2013;Fe. These features are also seen in the Fe&#x2013;LE binary systems (<xref ref-type="bibr" rid="B22">Ohmura et al., 2020</xref>). The results of densities and <italic>g</italic>&#x3b1;&#x3b2;(<italic>r</italic>) indicate that H, C, and O are interstitial, and that Si and S show substitutional properties in the liquid Fe&#x2013;LE&#x2013;O ternary systems as well as the liquid Fe&#x2013;LE binary systems.</p>
<fig id="F2" position="float">
<label>FIGURE 2</label>
<caption>
<p>Partial pair distribution functions of liquids <bold>(A)</bold> Fe<sub>160</sub>H<sub>20</sub>O<sub>20</sub> (Fe&#x2013;H&#x2013;O), <bold>(B)</bold> Fe<sub>160</sub>C<sub>20</sub>O<sub>20</sub> (Fe&#x2013;C&#x2013;O), <bold>(C)</bold> Fe<sub>160</sub>Si<sub>20</sub>O<sub>20</sub> (Fe&#x2013;Si&#x2013;O) and <bold>(D)</bold> Fe<sub>160</sub>S<sub>20</sub>O<sub>20</sub> (Fe&#x2013;S&#x2013;O) at 140&#xa0;GPa and 5000&#xa0;K.</p>
</caption>
<graphic xlink:href="feart-10-873088-g002.tif"/>
</fig>
<p>Regarding the LE&#x2013;LE interactions, we can see the different features of each liquid. For homoatomic interactions, H&#x2013;H does not have clear correlations. In contrast, C&#x2013;C shows strong interactions in the sense that there is a first peak at approximately 1.5&#xa0;&#xc5;, which is the smallest first peak position in all g&#x3b1;&#x3b2;(r). The strong C&#x2013;C interaction is found in liquid Fe&#x2013;C&#x2013;H system as well (<xref ref-type="bibr" rid="B5">Belonoshko et al., 2015</xref>). The first peak positions of <italic>g</italic>
<sub>O&#x2013;O</sub>(<italic>r</italic>) are almost the same as those of <italic>g</italic>
<sub>Fe&#x2013;Fe</sub>(<italic>r</italic>) in all liquids. However, the second&#x2013;peak positions are smaller than those of <italic>g</italic>
<sub>Fe&#x2013;Fe</sub>(<italic>r</italic>). For Si&#x2013;Si interactions, the first&#x2013;and second&#x2013;peak positions of Si&#x2013;Si are almost the same as those of Fe&#x2013;Fe or Fe&#x2013;Si. These features align with the results of earlier studies for liquid Fe&#x2013;O or Fe&#x2013;Si binary (<xref ref-type="bibr" rid="B2">Alfe et al., 1999</xref>; <xref ref-type="bibr" rid="B18">Morard et al., 2014</xref>; <xref ref-type="bibr" rid="B25">Posner and Steinle&#x2013;Neumann, 2019</xref>; <xref ref-type="bibr" rid="B22">Ohmura et al., 2020</xref>) and for Fe&#x2013;Si&#x2013;O ternary systems (<xref ref-type="bibr" rid="B27">Pozzo et al., 2013</xref>; <xref ref-type="bibr" rid="B4">Arveson et al., 2019</xref>; <xref ref-type="bibr" rid="B11">Huang et al., 2019</xref>). For S&#x2013;S interactions, the first peak is broad, and its position is much farther than those of other g&#x3b1;&#x3b2;(r) in liquid Fe&#x2013;S&#x2013;O. In terms of the heteroatomic interactions, H&#x2013;O, C&#x2013;O, and S&#x2013;O have similar behaviors in the sense that there are broad first peaks. In contrast, the first peak of <italic>g</italic>
<sub>Si&#x2013;O</sub>(<italic>r</italic>) is located at 1.8&#xa0;&#xc5; and sharp, meaning strong interactions between Si and O.</p>
</sec>
<sec id="s3-2">
<title>Bonding Properties</title>
<p>To clarify the detailed bonding nature in the liquid Fe&#x2013;LE&#x2013;O ternary systems, we use the Mulliken population analysis, where the electronic wave functions are expanded in an atomic orbital basis set (<xref ref-type="bibr" rid="B20">Mulliken, 1955</xref>; <xref ref-type="bibr" rid="B28">Shimojo et al., 2008</xref>). <xref ref-type="fig" rid="F3">Figure 3</xref> shows the time&#x2013;averaged distribution <inline-formula id="inf1">
<mml:math id="m1">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>&#x3b1;</mml:mi>
<mml:mi>&#x3b2;</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> of the bond overlap population <inline-formula id="inf2">
<mml:math id="m2">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mo>&#x2208;</mml:mo>
<mml:mi>&#x3b1;</mml:mi>
<mml:mo>,</mml:mo>
<mml:mi>j</mml:mi>
<mml:mo>&#x2208;</mml:mo>
<mml:mi>&#x3b2;</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula>, which gives a semiquantitative estimate of the covalent&#x2013;like bonding between the &#x3b1; and &#x3b2; atomic types in liquid Fe&#x2013;H&#x2013;O (A), Fe&#x2013;C&#x2013;O (B), Fe&#x2013;Si&#x2013;O (C), and Fe&#x2013;S&#x2013;O (D). It should be noted that, since the atomic&#x2013;orbital basis used in the expansion of the wavefunctions is not unique, the absolute magnitudes of <inline-formula id="inf3">
<mml:math id="m3">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> are little physical meaning. However, the trends remain unchanged for any choice of atomic&#x2013;orbital basis sets, and therefore we can discuss their relative variations meaningfully.</p>
<fig id="F3" position="float">
<label>FIGURE 3</label>
<caption>
<p>Distributions <inline-formula id="inf4">
<mml:math id="m4">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>&#x3b1;</mml:mi>
<mml:mi>&#x3b2;</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> of the overlap populations Oij for five pairs of &#x3b1;&#x2013;atomic and &#x3b2;&#x2013;atomic types of liquids <bold>(A)</bold> Fe-H-O, <bold>(B)</bold> Fe-C-O, <bold>(C)</bold> Fe-Si-O and <bold>(D)</bold> Fe-S-O. Thick solid, thin dashed, dotted dashed, double&#x2013;dotted dashed and thick dased lines show <inline-formula id="inf5">
<mml:math id="m5">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>&#x3b1;</mml:mi>
<mml:mi>&#x3b2;</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> for LE&#x2013;LE, Fe&#x2013;Fe, Fe&#x2013;LE, Fe&#x2013;O and LE&#x2013;O, respectively. Circles in Fe&#x2013;C&#x2013;O <bold>(B)</bold> and Fe&#x2013;<sub>Si&#x2013;O</sub> <bold>(C)</bold> show p<sub>C&#x2013;C</sub> <inline-formula id="inf6">
<mml:math id="m6">
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:math>
</inline-formula> and pSi&#x2013;Si <inline-formula id="inf7">
<mml:math id="m7">
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:math>
</inline-formula>, respectively. Squares show pSi&#x2013;O <inline-formula id="inf8">
<mml:math id="m8">
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:math>
</inline-formula> in liquid Fe&#x2013;Si&#x2013;O.</p>
</caption>
<graphic xlink:href="feart-10-873088-g003.tif"/>
</fig>
<p>
<xref ref-type="fig" rid="F3">Figure 3A</xref> shows <inline-formula id="inf9">
<mml:math id="m9">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>&#x3b1;</mml:mi>
<mml:mi>&#x3b2;</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> in liquid Fe&#x2013;H&#x2013;O. All of <inline-formula id="inf10">
<mml:math id="m10">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>&#x3b1;</mml:mi>
<mml:mi>&#x3b2;</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> in liquid Fe&#x2013;H&#x2013;O do not show strong overlaps. In contrast, as shown in <xref ref-type="fig" rid="F3">Figures 3B,C</xref>, <inline-formula id="inf11">
<mml:math id="m11">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>C</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>C</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula>, <inline-formula id="inf12">
<mml:math id="m12">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>S</mml:mi>
<mml:mi>i</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>S</mml:mi>
<mml:mi>i</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula>, and <inline-formula id="inf13">
<mml:math id="m13">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>S</mml:mi>
<mml:mi>i</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>O</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> have values in the regions <inline-formula id="inf14">
<mml:math id="m14">
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
</mml:math>
</inline-formula> &#x3e; 1.0, while other <inline-formula id="inf15">
<mml:math id="m15">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>&#x3b1;</mml:mi>
<mml:mi>&#x3b2;</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> are almost zero in the same region. For liquid Fe&#x2013;S&#x2013;O, <inline-formula id="inf16">
<mml:math id="m16">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>S</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>S</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> shows a relatively stronger interaction in the sense that there is a shoulder at approximately <inline-formula id="inf17">
<mml:math id="m17">
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
</mml:math>
</inline-formula> &#x3d; 0.5, but <inline-formula id="inf18">
<mml:math id="m18">
<mml:mrow>
<mml:msub>
<mml:mi>p</mml:mi>
<mml:mrow>
<mml:mi>S</mml:mi>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>S</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> &#x3d; 0 in the region <inline-formula id="inf19">
<mml:math id="m19">
<mml:mrow>
<mml:mover accent="true">
<mml:mi>O</mml:mi>
<mml:mo>&#xaf;</mml:mo>
</mml:mover>
</mml:mrow>
</mml:math>
</inline-formula> &#x3e; 1.0. Although the Si&#x2013;O and Si&#x2013;Si atomic distances are almost the same as those for Fe&#x2013;O and Fe&#x2013;Fe, respectively (<xref ref-type="fig" rid="F2">Figure 2C</xref>), the bonding nature is different. Covalency are clearly found between Si&#x2013;O and Si&#x2013;Si, whereas not between Fe&#x2013;O and Fe&#x2013;Fe. These results indicate that C&#x2013;C, Si&#x2013;Si, and Si&#x2013;O have covalent&#x2013;like interactions in liquid Fe mixtures even under high&#x2013;pressure conditions (&#x3e;100&#xa0;GPa).</p>
<p>In order to analyze the covalent&#x2013;like interactions of C&#x2013;C, Si&#x2013;Si, and Si&#x2013;O in more detail, we investigate the time evolution of the bond overlap population <inline-formula id="inf20">
<mml:math id="m20">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula>. <xref ref-type="fig" rid="F4">Figure 4</xref> shows <inline-formula id="inf21">
<mml:math id="m21">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>C</mml:mtext>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>C</mml:mtext>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> (overlap population between C1 and C2 atoms) displayed with the time evolution of the atomic distance between C1 and C2 atoms, <italic>d</italic>
<sub>C1&#x2013;C2</sub>(<italic>t</italic>), and the snapshots of atomic configurations. At <italic>t</italic> &#x3d; 0.00&#xa0;ps, <italic>d</italic>
<sub>C1&#x2013;C2</sub>(<italic>t</italic>) is more than 2.0&#xa0;&#xc5; and <inline-formula id="inf22">
<mml:math id="m22">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>C</mml:mi>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>C</mml:mi>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
<mml:mo>&#xa0;</mml:mo>
</mml:mrow>
</mml:math>
</inline-formula> is zero, meaning no covalent bonding between C1 and C2. <inline-formula id="inf23">
<mml:math id="m23">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>C</mml:mi>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>C</mml:mi>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> increases when <italic>d</italic>
<sub>C1&#x2013;C2</sub>(<italic>t</italic>) decreases, meaning that a covalent bond forms between C1 and C2 (the snapshot at t &#x3d; 0.13&#xa0;ps). After <inline-formula id="inf24">
<mml:math id="m24">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>C</mml:mi>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>C</mml:mi>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> and <italic>d</italic>
<sub>C1&#x2013;C2</sub>(<italic>t</italic>) oscillate approximately 10 times, <inline-formula id="inf25">
<mml:math id="m25">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>C</mml:mi>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>C</mml:mi>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> becomes almost 0 and <italic>d</italic>
<sub>C1&#x2013;C2</sub>(<italic>t</italic>) becomes more than 2.5&#xa0;&#xc5; at approximately 0.40&#xa0;ps, meaning that the covalent bond between C1 and C2 is lost, as shown in the snapshot at t &#x3d; 0.40&#xa0;ps. From the result, the lifetime of the C&#x2013;C covalent bond is estimated to be approximately 0.3&#xa0;ps at this P,T.</p>
<fig id="F4" position="float">
<label>FIGURE 4</label>
<caption>
<p>
<bold>(A)</bold> The time evolution of atomic distance between C1 and C2, <italic>d</italic>
<sub>C1&#x2013;C2</sub>(<italic>t</italic>), and <bold>(B)</bold> the overlap population, <inline-formula id="inf26">
<mml:math id="m26">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>C</mml:mtext>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>C</mml:mtext>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> (Thick solid line). Dashed lines show <inline-formula id="inf27">
<mml:math id="m27">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>C</mml:mtext>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>Fe</mml:mtext>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula>. <bold>(C)</bold> Atomic configurations around C1 and C2 at t &#x3d; 0.00, 0.13, 0.30 and 0.40 ps. The pink, green and red spheres correspond to Fe, C and O atoms, respectively. The dark spheres represent Fe atoms that are in the process of moving outside the frame, and towards the paper boundary.</p>
</caption>
<graphic xlink:href="feart-10-873088-g004.tif"/>
</fig>
<p>
<xref ref-type="fig" rid="F5">Figure 5</xref> shows the time evolution of the distance and overlap population of focusing atomic pair (Si1 and Si2), <italic>d</italic>Si1&#x2013;Si2(t) and the <inline-formula id="inf28">
<mml:math id="m28">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>Si</mml:mtext>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>Si</mml:mtext>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula>, with the snapshots of atomic configuration in liquid Fe&#x2013;Si&#x2013;O. At t &#x3d; 0.00 ps, dSi1&#x2013;Si2(t) is almost 3.5&#xa0;&#xc5;, and <inline-formula id="inf29">
<mml:math id="m29">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>Si</mml:mtext>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>Si</mml:mtext>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> is almost 0. Similar to the C&#x2013;C interactions shown in <xref ref-type="fig" rid="F4">Figure 4</xref>, with time, an Si&#x2013;Si covalent&#x2013;like bond forms (the snapshot at 0.70&#xa0;ps), and the Si&#x2013;Si bond oscillates several times, then the bond dissolves (at 1.30&#xa0;ps).</p>
<fig id="F5" position="float">
<label>FIGURE 5</label>
<caption>
<p>
<bold>(A)</bold> The time evolution of atomic distance between Si1 and Si2, <italic>d</italic>
<sub>Si1&#x2013;Si2</sub>(<italic>t</italic>), and <bold>(B)</bold> the overlap population, <inline-formula id="inf30">
<mml:math id="m30">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>Si</mml:mtext>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>Si</mml:mtext>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> (Thick solid line). Dashed lines show <inline-formula id="inf31">
<mml:math id="m31">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>Si</mml:mtext>
<mml:mn>1</mml:mn>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>Fe</mml:mtext>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula>. <bold>(C)</bold> Atomic configurations around Si1 and Si2 at t &#x3d; 0.00, 0.70 and 1.30 ps. The pink, yellow and red spheres correspond to Fe, Si and O atoms, respectively.</p>
</caption>
<graphic xlink:href="feart-10-873088-g005.tif"/>
</fig>
<p>In liquid Fe&#x2013;Si&#x2013;O, Si&#x2013;O covalent bonding can also be observed. OSi&#x2013;O(t), dSi&#x2013;O(t), and snapshots of the atomic configuration are shown in <xref ref-type="fig" rid="F6">Figure 6</xref>. At t &#x3d; 0.00&#xa0;ps, OSi&#x2013;O(t) is almost 0, meaning no covalent bond between Si and O (the snapshot at t &#x3d; 0.00&#xa0;ps). OSi&#x2013;O(t) begins to increase at approximately 0.05&#xa0;ps, meaning the covalent bond formation between Si and O. Similar to C&#x2013;C and Si&#x2013;Si covalent bonds, after the Si&#x2013;O bond oscillates several times, OSi&#x2013;O(t) decreases drastically at approximately 0.22&#xa0;ps. At the same time. dSi&#x2013;O(t) increases, meaning that covalent bond between Si&#x2013;O dissolves (the snapshot at 0.25&#xa0;ps). From this result, we can estimate the lifetime of the Si&#x2013;O covalent bond to be approximately 0.15&#xa0;ps at this <italic>P</italic>,<italic>T</italic>.</p>
<fig id="F6" position="float">
<label>FIGURE 6</label>
<caption>
<p>
<bold>(A)</bold> The time evolution of distance between Si and O atoms, <italic>d</italic>
<sub>Si&#x2013;O</sub>(<italic>t</italic>), and <bold>(B)</bold> the overlap population <inline-formula id="inf32">
<mml:math id="m32">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>Si</mml:mtext>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>O</mml:mtext>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula> (Thick solid line). Dashed lines show <inline-formula id="inf33">
<mml:math id="m33">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mtext>Si</mml:mtext>
<mml:mo>&#x2212;</mml:mo>
<mml:mtext>Fe</mml:mtext>
</mml:mrow>
</mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mi>t</mml:mi>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
</inline-formula>. <bold>(C)</bold> Atomic configurations around Si and O at t &#x3d; 0.00, 0.06, 0.12 and 0.25 ps. The pink, yellow and red spheres correspond to Fe, Si and O atoms, respectively.</p>
</caption>
<graphic xlink:href="feart-10-873088-g006.tif"/>
</fig>
<p>Our calculations clearly indicate that in liquid Fe&#x2013;Si&#x2013;O and Fe&#x2013;C&#x2013;O, covalent&#x2013;like interactions with finite lifetimes exist between C and C, Si and Si, and also Si and O under high&#x2013;pressure more than 100&#xa0;GPa.</p>
<p>Charge distribution of Si atoms in liquid Fe&#x2013;Si&#x2013;O.</p>
<p>
<xref ref-type="fig" rid="F7">Figure 7A</xref> shows the averaged distribution <italic>q</italic>&#x3b1;(<italic>Q</italic>) of the gross charge <inline-formula id="inf34">
<mml:math id="m34">
<mml:mrow>
<mml:msub>
<mml:mi>Q</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mo>&#x2208;</mml:mo>
<mml:mi>&#x3b1;</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> for &#x3b1; type atoms in liquid Fe&#x2013;Si&#x2013;O obtained by population analysis as same as <inline-formula id="inf35">
<mml:math id="m35">
<mml:mrow>
<mml:msub>
<mml:mi>O</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula>. As shown in <xref ref-type="fig" rid="F7">Figure 7A</xref>, the peak positions of <italic>q</italic>
<sub>Fe</sub>(<italic>Q</italic>), <italic>q</italic>
<sub>Si</sub>(<italic>Q</italic>), and <italic>q</italic>
<sub>O</sub>(<italic>Q</italic>) are approximately <italic>Q</italic> &#x3d; 0.1, &#x2013;0.2, and &#x2013;0.7, respectively. While the Si&#x2013;O covalent bond affects the atomic charge of the Si atom, the C&#x2013;C and Si&#x2013;Si interactions have no effects on the atomic charge of C and Si (<xref ref-type="sec" rid="s9">Supplementary Figure S2</xref>). To analyze <italic>q</italic>
<sub>Si</sub>(<italic>Q</italic>) in more detail, we decompose <italic>q</italic>
<sub>Si</sub>(<italic>Q</italic>) into <italic>q</italic>
<sub>Si&#x2013;O</sub>(<italic>Q</italic>) and <italic>q</italic>
<sub>Si&#x2013;nonO</sub>(<italic>Q</italic>). Here, <italic>q</italic>
<sub>Si&#x2013;O</sub>(<italic>Q</italic>) means the distribution of the atomic charge for Si atoms coordinated to O atoms, which is displayed as a thick dashed line in <xref ref-type="fig" rid="F7">Figure 7B</xref> and <italic>q</italic>
<sub>Si&#x2013;nonO</sub>(<italic>Q</italic>) means the distribution of the atomic charge for Si atoms unbonded to O atoms, which is displayed as a thin solid line in <xref ref-type="fig" rid="F7">Figure 7B</xref>. As shown in <xref ref-type="fig" rid="F7">Figure 7B</xref>, <italic>q</italic>
<sub>Si&#x2013;O</sub>(<italic>Q</italic>) is distributed to a relatively large Q region, which means that Si atoms have more positive charges when bonded to the O atom compared to the charges when the Si atoms are unbonded to O.</p>
<fig id="F7" position="float">
<label>FIGURE 7</label>
<caption>
<p>
<bold>(A)</bold> The distribution of <italic>q</italic>&#x3b1;(<italic>Q</italic>) of the gross charges <inline-formula id="inf36">
<mml:math id="m36">
<mml:mrow>
<mml:msub>
<mml:mi>Q</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mo>&#xa0;</mml:mo>
<mml:mo>&#x2208;</mml:mo>
<mml:mo>&#xa0;</mml:mo>
<mml:mtext>&#x3b1;</mml:mtext>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula>. The thin solid, thick solid and dashed lines represent <italic>q</italic>
<sub>Fe</sub>(<italic>Q</italic>), <italic>q</italic>
<sub>Si</sub>(<italic>Q</italic>) and <italic>q</italic>
<sub>O</sub>(<italic>Q</italic>), respectively. <bold>(B)</bold> The distribution of <italic>q</italic>
<sub>Si</sub>(<italic>Q</italic>) decomposed into <italic>q</italic>
<sub>Si&#x2013;O</sub>(<italic>Q</italic>) and <italic>q</italic>
<sub>Si&#x2013;nonO</sub>(<italic>Q</italic>). The former represents the charge distribution for Si atoms coordinated to O atoms (a pink thin&#x2013;dashed line) and the latter represents the charge distribution of Si atoms unbonded to O atoms (a brown thin&#x2013;solid line).</p>
</caption>
<graphic xlink:href="feart-10-873088-g007.tif"/>
</fig>
<p>According to an earlier study (<xref ref-type="bibr" rid="B4">Arveson et al., 2019</xref>), liquid Fe&#x2013;Si&#x2013;O shows might have immiscibility between liquid Fe&#x2013;Si&#x2013;O and Fe&#x2013;Si (there are two domains with and without oxygen in liquid Fe&#x2013;Si&#x2013;O) just above their solidus temperatures at Earth&#x2019;s outer core pressures. Atomic configurations in our simulation also seem to be suggestive of this phase separation though the actual immiscibility region might exist at some lower temperatures (<xref ref-type="sec" rid="s9">Supplementary Figure S3</xref>). The shift of atomic charge due to the Si&#x2013;O covalent bond is possibly related to the gathering of oxygen atoms with negative charges around Si, leading to the separation of ionic Fe&#x2013;Si&#x2013;O and metallic Fe&#x2013;Si domains in liquid Fe&#x2013;Si&#x2013;O. However, at the moment, the upper temperature bound of the immiscibility region at the outer core pressures is yet to be determined. In addition to these atomic perspectives, energetic information regarding thermodynamic stability of miscible and immiscible liquids has to be determined to understand the immiscibility of liquid Fe&#x2013;Si&#x2013;O in more detail.</p>
</sec>
</sec>
<sec id="s4">
<title>4 Conclusion</title>
<p>The structural and bonding properties of liquid Fe&#x2013;H&#x2013;O, Fe&#x2013;C&#x2013;O, Fe&#x2013;Si&#x2013;O and Fe&#x2013;S&#x2013;O ternary systems under high pressure have been investigated by ab initio molecular&#x2013;dynamics simulations. The pair distribution functions indicated the interstitial nature for H, C, and O but the substitutional one for Si and S, similar to liquid Fe&#x2013;LE binary systems. Regarding the interactions between light elements, bond&#x2013;overlap populations showed covalent characters in C&#x2013;C, Si&#x2013;Si, and Si&#x2013;O interactions in liquid Fe&#x2013;C&#x2013;O and Fe&#x2013;Si&#x2013;O even under high&#x2013;pressure condition. Mulliken charge analyses clarified that the Si&#x2013;O covalent bond caused a shift in the atomic charge of Si to more positive. This might be related to the phase separation between the Fe&#x2013;Si&#x2013;O and Fe&#x2013;Si domains in liquid Fe&#x2013;Si&#x2013;O. To further understand immiscibility of multi&#x2013;component liquid Fe mixtures such as liquid Fe&#x2013;Si&#x2013;O, thermodynamic stability should be explored.</p>
</sec>
</body>
<back>
<sec id="s5">
<title>Data Availability Statement</title>
<p>The original contributions presented in the study are included in the article/<xref ref-type="sec" rid="s9">Supplementary Material</xref>, further inquiries can be directed to the corresponding author.</p>
</sec>
<sec id="s6">
<title>Author Contributions</title>
<p>SO: Methodology, formal analysis, investigation, writing&#x2013;original draft, project administration. FS: Software, writing&#x2013;review and editing. TT: Validation, supervision, writing&#x2013;review and editing.</p>
</sec>
<sec id="s7">
<title>Funding</title>
<p>This work was supported by KAKENHI (Nos. 21K03705 and 20H00198).</p>
</sec>
<sec sec-type="COI-statement" id="s8">
<title>Conflict of Interest</title>
<p>The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.</p>
</sec>
<sec sec-type="disclaimer" id="s9">
<title>Publisher&#x2019;s Note</title>
<p>All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.</p>
</sec>
<ack>
<p>The authors thank the Supercomputer Center, Institute for Solid State Physics, the University of Tokyo for the use of the facilities. The computation was also carried out using the computer facilities at the Research Institute for Information Technology, Kyushu University.</p>
</ack>
<sec id="s10">
<title>Supplementary Material</title>
<p>The Supplementary Material for this article can be found online at: <ext-link ext-link-type="uri" xlink:href="https://www.frontiersin.org/articles/10.3389/feart.2022.873088/full#supplementary-material">https://www.frontiersin.org/articles/10.3389/feart.2022.873088/full&#x23;supplementary&#x2013;material</ext-link>
</p>
<supplementary-material xlink:href="DataSheet1.PDF" id="SM1" mimetype="application/PDF" xmlns:xlink="http://www.w3.org/1999/xlink"/>
</sec>
<ref-list>
<title>References</title>
<ref id="B1">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Alfe</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Gillan</surname>
<given-names>M. J.</given-names>
</name>
</person-group> (<year>1998</year>). <article-title>First&#x2013;principles Simulations of Liquid Fe&#x2013;S under Earth&#x27;s Core Conditions</article-title>. <source>Phys. Rev. B</source> <volume>58</volume>, <fpage>8248</fpage>&#x2013;<lpage>8256</lpage>. <pub-id pub-id-type="doi">10.1103/physrevb.58.8248</pub-id> </citation>
</ref>
<ref id="B2">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Alfe</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Price</surname>
<given-names>G. D.</given-names>
</name>
<name>
<surname>Gillan</surname>
<given-names>M. J.</given-names>
</name>
</person-group> (<year>1999</year>). <article-title>Oxygen in the Earth&#x0027;s Core: a First&#x2013;Principles Study</article-title>. <source>Phys. Earth Planet. Inter.</source> <volume>110</volume>, <fpage>191</fpage>&#x2013;<lpage>210</lpage>. <pub-id pub-id-type="doi">10.1016/s0031&#x2013;9201(98)00134&#x2013;4</pub-id> </citation>
</ref>
<ref id="B3">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Anderson</surname>
<given-names>O. L.</given-names>
</name>
<name>
<surname>Isaak</surname>
<given-names>D. G.</given-names>
</name>
</person-group> (<year>2002</year>). <article-title>Another Look at the Core Density Deficit of Earth&#x27;s Outer Core</article-title>. <source>Phys. Earth Planet. Interiors</source> <volume>131</volume>, <fpage>19</fpage>&#x2013;<lpage>27</lpage>. <pub-id pub-id-type="doi">10.1016/s0031&#x2013;9201(02)00017&#x2013;1</pub-id> </citation>
</ref>
<ref id="B4">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Arveson</surname>
<given-names>S. M.</given-names>
</name>
<name>
<surname>Deng</surname>
<given-names>J.</given-names>
</name>
<name>
<surname>Karki</surname>
<given-names>B. B.</given-names>
</name>
<name>
<surname>Lee</surname>
<given-names>K. K. M.</given-names>
</name>
</person-group> (<year>2019</year>). <article-title>Evidence for Fe&#x2013;Si&#x2013;O Liquid Immiscibility at Deep Earth Pressures</article-title>. <source>Proc. Natl. Acad. Sci. U.S.A.</source> <volume>116</volume>, <fpage>10238</fpage>&#x2013;<lpage>10243</lpage>. <pub-id pub-id-type="doi">10.1073/pnas.1821712116</pub-id> </citation>
</ref>
<ref id="B5">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Belonoshko</surname>
<given-names>A. B.</given-names>
</name>
<name>
<surname>Lukinov</surname>
<given-names>T.</given-names>
</name>
<name>
<surname>Rosengren</surname>
<given-names>A.</given-names>
</name>
<name>
<surname>Bryk</surname>
<given-names>T.</given-names>
</name>
<name>
<surname>Litasov</surname>
<given-names>K. D.</given-names>
</name>
</person-group> (<year>2015</year>). <article-title>Synthesis of Heavy Hydrocarbons at the Core&#x2013;Mantle Boundary</article-title>. <source>Sci. Rep.</source> <volume>5</volume>, <fpage>18382</fpage>&#x2013;<lpage>18416</lpage>. <pub-id pub-id-type="doi">10.1038/srep18382</pub-id> </citation>
</ref>
<ref id="B6">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Birch</surname>
<given-names>F.</given-names>
</name>
</person-group> (<year>1964</year>). <article-title>Density and Composition of Mantle and Core</article-title>. <source>J. Geophys. Res.</source> <volume>69</volume>, <fpage>4377</fpage>&#x2013;<lpage>4388</lpage>. <pub-id pub-id-type="doi">10.1029/jz069i020p04377</pub-id> </citation>
</ref>
<ref id="B7">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Bl&#xf6;chl</surname>
<given-names>P. E.</given-names>
</name>
</person-group> (<year>1994</year>). <article-title>Projector Augmented&#x2013;Wave Method</article-title>. <source>Phys. Rev. B</source> <volume>50</volume>, <fpage>17953</fpage>&#x2013;<lpage>17979</lpage>. <pub-id pub-id-type="doi">10.1021/acs.jctc.7b00404.s001</pub-id> </citation>
</ref>
<ref id="B8">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>De Koker</surname>
<given-names>N.</given-names>
</name>
<name>
<surname>Steinle&#x2013;Neumann</surname>
<given-names>G.</given-names>
</name>
<name>
<surname>Vl&#x10d;ek</surname>
<given-names>V.</given-names>
</name>
</person-group> (<year>2012</year>). <article-title>Electrical Resistivity and thermal Conductivity of Liquid Fe Alloys at High P and T , and Heat Flux in Earth&#x27;s Core</article-title>. <source>Proc. Natl. Acad. Sci. U.S.A.</source> <volume>109</volume>, <fpage>4070</fpage>&#x2013;<lpage>4073</lpage>. <pub-id pub-id-type="doi">10.1073/pnas.1111841109</pub-id> </citation>
</ref>
<ref id="B9">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Helffrich</surname>
<given-names>G.</given-names>
</name>
<name>
<surname>Kaneshima</surname>
<given-names>S.</given-names>
</name>
</person-group> (<year>2004</year>). <article-title>Seismological Constraints on Core Composition from Fe&#x2013;O&#x2013;S Liquid Immiscibility</article-title>. <source>Science</source> <volume>306</volume>, <fpage>2239</fpage>&#x2013;<lpage>2242</lpage>. <pub-id pub-id-type="doi">10.1126/science.1101109</pub-id> </citation>
</ref>
<ref id="B10">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Hoover</surname>
<given-names>W. G.</given-names>
</name>
</person-group> (<year>1985</year>). <article-title>Canonical Dynamics: Equilibrium Phase&#x2013;Space Distributions</article-title>. <source>Phys. Rev. A.</source> <volume>31</volume>, <fpage>1695</fpage>&#x2013;<lpage>1697</lpage>. <pub-id pub-id-type="doi">10.1103/physreva.31.1695</pub-id> </citation>
</ref>
<ref id="B11">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Huang</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Badro</surname>
<given-names>J.</given-names>
</name>
<name>
<surname>Brodholt</surname>
<given-names>J.</given-names>
</name>
<name>
<surname>Li</surname>
<given-names>Y.</given-names>
</name>
</person-group> (<year>2019</year>). <article-title>Ab Initio Molecular Dynamics Investigation of Molten Fe&#x2013;Si&#x2013;O in Earth&#x27;s Core</article-title>. <source>Geophys. Res. Lett.</source> <volume>46</volume>, <fpage>6397</fpage>&#x2013;<lpage>6405</lpage>. <pub-id pub-id-type="doi">10.1029/2019gl082722</pub-id> </citation>
</ref>
<ref id="B12">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Ichikawa</surname>
<given-names>H.</given-names>
</name>
<name>
<surname>Tsuchiya</surname>
<given-names>T.</given-names>
</name>
</person-group> (<year>2015</year>). <article-title>Atomic Transport Property of Fe&#x2013;O Liquid Alloys in the Earth&#x27;s Outer Core P, T Condition</article-title>. <source>Phys. Earth Planet. Interiors</source> <volume>247</volume>, <fpage>27</fpage>&#x2013;<lpage>35</lpage>. <pub-id pub-id-type="doi">10.1016/j.pepi.2015.03.006</pub-id> </citation>
</ref>
<ref id="B13">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Keeler</surname>
<given-names>R. N.</given-names>
</name>
<name>
<surname>Royce</surname>
<given-names>E. B.</given-names>
</name>
</person-group> (<year>1971</year>). <article-title>Shock Waves in Condensed mediaPhysics of High Energy Density</article-title>. <source>Proc. Int. Sch. Phys. "Enrico Fermi", Course</source> <volume>XLVIII</volume>, <fpage>51</fpage>. </citation>
</ref>
<ref id="B14">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Kresse</surname>
<given-names>G.</given-names>
</name>
<name>
<surname>Hafner</surname>
<given-names>J.</given-names>
</name>
</person-group> (<year>1994</year>). <article-title>Ab Initiomolecular&#x2013;Dynamics Simulation of the Liquid&#x2013;Metal&#x2013;Amorphous&#x2013;Semiconductor Transition in Germanium</article-title>. <source>Phys. Rev. B</source> <volume>49</volume>, <fpage>14251</fpage>&#x2013;<lpage>14269</lpage>. <pub-id pub-id-type="doi">10.1103/physrevb.49.14251</pub-id> </citation>
</ref>
<ref id="B15">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Kresse</surname>
<given-names>G.</given-names>
</name>
<name>
<surname>Joubert</surname>
<given-names>D.</given-names>
</name>
</person-group> (<year>1999</year>). <article-title>From Ultrasoft Pseudopotentials to the Projector Augmented&#x2013;Wave Method</article-title>. <source>Phys. Rev. B</source> <volume>59</volume>, <fpage>1758</fpage>&#x2013;<lpage>1775</lpage>. <pub-id pub-id-type="doi">10.1103/physrevb.59.1758</pub-id> </citation>
</ref>
<ref id="B16">
<citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname>Matassov</surname>
<given-names>G.</given-names>
</name>
</person-group> (<year>1977</year>). <source>Electrical Conductivity of Iron&#x2013;&#x2013;silicon alloys at high pressures and the earth&#x27;s core</source>. <publisher-loc>Livermore (USA)United States)</publisher-loc>: <publisher-name>California Univ.Lawrence Livermore Lab.</publisher-name> </citation>
</ref>
<ref id="B17">
<citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname>Mcdonough</surname>
<given-names>W. F.</given-names>
</name>
</person-group> (<year>2003</year>). &#x201c;<article-title>Compositional Model for the Earth&#x0027;s Core</article-title>&#x201d; in <source>Treatise on Geochemistry</source>. Editor <person-group person-group-type="editor">
<name>
<surname>Turekian</surname>
<given-names>K. K.</given-names>
</name>
</person-group> (<publisher-loc>Oxford</publisher-loc>: <publisher-name>Pergamon</publisher-name>), <fpage>547</fpage>&#x2013;<lpage>568</lpage>. <pub-id pub-id-type="doi">10.1016/b0&#x2013;08&#x2013;043751&#x2013;6/02015&#x2013;6</pub-id> </citation>
</ref>
<ref id="B18">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Morard</surname>
<given-names>G.</given-names>
</name>
<name>
<surname>Andrault</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Antonangeli</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Bouchet</surname>
<given-names>J.</given-names>
</name>
</person-group> (<year>2014</year>). <article-title>Properties of Iron Alloys under the Earth&#x27;s Core Conditions</article-title>. <source>Comptes Rendus Geosci.</source> <volume>346</volume>, <fpage>130</fpage>&#x2013;<lpage>139</lpage>. <pub-id pub-id-type="doi">10.1016/j.crte.2014.04.007</pub-id> </citation>
</ref>
<ref id="B19">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Morard</surname>
<given-names>G.</given-names>
</name>
<name>
<surname>Nakajima</surname>
<given-names>Y.</given-names>
</name>
<name>
<surname>Andrault</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Antonangeli</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Auzende</surname>
<given-names>A. L.</given-names>
</name>
<name>
<surname>Boulard</surname>
<given-names>E.</given-names>
</name>
<etal/>
</person-group> (<year>2017</year>). <article-title>Structure and Density of Fe&#x2013;C Liquid Alloys under High Pressure</article-title>. <source>J. Geophys. Res. Solid Earth</source> <volume>122</volume>, <fpage>7813</fpage>&#x2013;<lpage>7823</lpage>. <pub-id pub-id-type="doi">10.1002/2017jb014779</pub-id> </citation>
</ref>
<ref id="B20">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Mulliken</surname>
<given-names>R. S.</given-names>
</name>
</person-group> (<year>1955</year>). <article-title>Electronic Population Analysis on LCAO&#x2013;MO Molecular Wave Functions. II. Overlap Populations, Bond Orders, and Covalent Bond Energies</article-title>. <source>J. Chem. Phys.</source> <volume>23</volume>, <fpage>1841</fpage>&#x2013;<lpage>1846</lpage>. <pub-id pub-id-type="doi">10.1063/1.1740589</pub-id> </citation>
</ref>
<ref id="B21">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Nos&#xe9;</surname>
<given-names>S.</given-names>
</name>
</person-group> (<year>1984</year>). <article-title>A Molecular Dynamics Method for Simulations in the Canonical Ensemble</article-title>. <source>Mol. Phys.</source> <volume>52</volume>, <fpage>255</fpage>&#x2013;<lpage>268</lpage>. <pub-id pub-id-type="doi">10.1080/00268978400101201</pub-id> </citation>
</ref>
<ref id="B22">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Ohmura</surname>
<given-names>S.</given-names>
</name>
<name>
<surname>Tsuchiya</surname>
<given-names>T.</given-names>
</name>
<name>
<surname>Shimojo</surname>
<given-names>F.</given-names>
</name>
</person-group> (<year>2020</year>). <article-title>Structures of Liquid Iron&#x2013;Light Element Mixtures under High Pressure</article-title>. <source>Phys. Status Solidi B</source> <volume>257</volume>, <fpage>2000098</fpage>. <pub-id pub-id-type="doi">10.1002/pssb.202000098</pub-id> </citation>
</ref>
<ref id="B23">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Perdew</surname>
<given-names>J. P.</given-names>
</name>
<name>
<surname>Burke</surname>
<given-names>K.</given-names>
</name>
<name>
<surname>Ernzerhof</surname>
<given-names>M.</given-names>
</name>
</person-group> (<year>1996</year>). <article-title>Generalized Gradient Approximation Made Simple</article-title>. <source>Phys. Rev. Lett.</source> <volume>77</volume>, <fpage>3865</fpage>&#x2013;<lpage>3868</lpage>. <pub-id pub-id-type="doi">10.1103/physrevlett.77.3865</pub-id> </citation>
</ref>
<ref id="B24">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Poirier</surname>
<given-names>J.&#x2013;P.</given-names>
</name>
</person-group> (<year>1994</year>). <article-title>Light Elements in the Earth&#x27;s Outer Core: A Critical Review</article-title>. <source>Phys. Earth Planet. Interiors</source> <volume>85</volume>, <fpage>319</fpage>&#x2013;<lpage>337</lpage>. <pub-id pub-id-type="doi">10.1016/0031&#x2013;9201(94)90120&#x2013;1</pub-id> </citation>
</ref>
<ref id="B25">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Posner</surname>
<given-names>E. S.</given-names>
</name>
<name>
<surname>Steinle-Neumann</surname>
<given-names>G.</given-names>
</name>
</person-group> (<year>2019</year>). <article-title>Mass Transport and Structural Properties of Binary Liquid Iron Alloys at High Pressure</article-title>. <source>Geochem. Geophys. Geosyst.</source> <volume>20</volume>, <fpage>3556</fpage>&#x2013;<lpage>3568</lpage>. <pub-id pub-id-type="doi">10.1029/2019gc008393</pub-id> </citation>
</ref>
<ref id="B26">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Pozzo</surname>
<given-names>M.</given-names>
</name>
<name>
<surname>Davies</surname>
<given-names>C.</given-names>
</name>
<name>
<surname>Gubbins</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Alfe</surname>
<given-names>D.</given-names>
</name>
</person-group> (<year>2012</year>). <article-title>Thermal and Electrical Conductivity of Iron at Earth&#x27;s Core Conditions</article-title>. <source>Nature</source> <volume>485</volume>, <fpage>355</fpage>&#x2013;<lpage>358</lpage>. <pub-id pub-id-type="doi">10.1038/nature11031</pub-id> </citation>
</ref>
<ref id="B27">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Pozzo</surname>
<given-names>M.</given-names>
</name>
<name>
<surname>Davies</surname>
<given-names>C.</given-names>
</name>
<name>
<surname>Gubbins</surname>
<given-names>D.</given-names>
</name>
<name>
<surname>Alfe</surname>
<given-names>D.</given-names>
</name>
</person-group> (<year>2013</year>). <article-title>Transport Properties for Liquid Silicon&#x2013;Oxygen&#x2013;Iron Mixtures at Earth&#x27;s Core Conditions</article-title>. <source>Phys. Rev. B</source> <volume>87</volume>, <fpage>014110</fpage>. <pub-id pub-id-type="doi">10.1103/physrevb.87.014110</pub-id> </citation>
</ref>
<ref id="B28">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Shimojo</surname>
<given-names>F.</given-names>
</name>
<name>
<surname>Nakano</surname>
<given-names>A.</given-names>
</name>
<name>
<surname>Kalia</surname>
<given-names>R. K.</given-names>
</name>
<name>
<surname>Vashishta</surname>
<given-names>P.</given-names>
</name>
</person-group> (<year>2008</year>). <article-title>Electronic Processes in Fast Thermite Chemical Reactions: A First&#x2013;Principles Molecular Dynamics Study</article-title>. <source>Phys. Rev. E Stat. Nonlin Soft Matter Phys.</source> <volume>77</volume>, <fpage>066103</fpage>. <pub-id pub-id-type="doi">10.1103/PhysRevE.77.066103</pub-id> </citation>
</ref>
<ref id="B29">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Shimojo</surname>
<given-names>F.</given-names>
</name>
<name>
<surname>Kalia</surname>
<given-names>R. K.</given-names>
</name>
<name>
<surname>Nakano</surname>
<given-names>A.</given-names>
</name>
<name>
<surname>Vashishta</surname>
<given-names>P.</given-names>
</name>
</person-group> (<year>2001</year>). <article-title>Linear&#x2013;scaling Density&#x2013;Functional&#x2013;Theory Calculations of Electronic Structure Based on Real&#x2013;Space Grids: Design, Analysis, and Scalability Test of Parallel Algorithms</article-title>. <source>Comput. Phys. Commun.</source> <volume>140</volume>, <fpage>303</fpage>&#x2013;<lpage>314</lpage>. <pub-id pub-id-type="doi">10.1016/s0010&#x2013;4655(01)00247&#x2013;8</pub-id> </citation>
</ref>
<ref id="B30">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Stacey</surname>
<given-names>F. D.</given-names>
</name>
<name>
<surname>Anderson</surname>
<given-names>O. L.</given-names>
</name>
</person-group> (<year>2001</year>). <article-title>Electrical and thermal Conductivities of Fe&#x2013;Ni&#x2013;Si alloy under Core Conditions</article-title>. <source>Phys. Earth Planet. Interiors</source> <volume>124</volume>, <fpage>153</fpage>&#x2013;<lpage>162</lpage>. <pub-id pub-id-type="doi">10.1016/s0031&#x2013;9201(01)00186&#x2013;8</pub-id> </citation>
</ref>
<ref id="B31">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Tsuno</surname>
<given-names>K.</given-names>
</name>
<name>
<surname>Ohtani</surname>
<given-names>E.</given-names>
</name>
<name>
<surname>Terasaki</surname>
<given-names>H.</given-names>
</name>
</person-group> (<year>2007</year>). <article-title>Immiscible Two&#x2013;Liquid Regions in the Fe&#x2013;O&#x2013;S System at High Pressure: Implications for Planetary Cores</article-title>. <source>Phys. Earth Planet. Interiors</source> <volume>160</volume>, <fpage>75</fpage>&#x2013;<lpage>85</lpage>. <pub-id pub-id-type="doi">10.1016/j.pepi.2006.09.004</pub-id> </citation>
</ref>
<ref id="B32">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Tuckerman</surname>
<given-names>M.</given-names>
</name>
<name>
<surname>Berne</surname>
<given-names>B. J.</given-names>
</name>
<name>
<surname>Martyna</surname>
<given-names>G. J.</given-names>
</name>
</person-group> (<year>1992</year>). <article-title>Reversible Multiple Time Scale Molecular Dynamics</article-title>. <source>J. Chem. Phys.</source> <volume>97</volume>, <fpage>1990</fpage>&#x2013;<lpage>2001</lpage>. <pub-id pub-id-type="doi">10.1063/1.463137</pub-id> </citation>
</ref>
<ref id="B33">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Wagle</surname>
<given-names>F.</given-names>
</name>
<name>
<surname>Steinle&#x2013;Neumann</surname>
<given-names>G.</given-names>
</name>
<name>
<surname>De Koker</surname>
<given-names>N.</given-names>
</name>
</person-group> (<year>2018</year>). <article-title>Saturation and Negative Temperature Coefficient of Electrical Resistivity in Liquid Iron&#x2013;Sulfur Alloys at High Densities from First&#x2013;Principles Calculations</article-title>. <source>Phys. Rev. B</source> <volume>97</volume>, <fpage>094307</fpage>. <pub-id pub-id-type="doi">10.1103/physrevb.97.094307</pub-id> </citation>
</ref>
<ref id="B34">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Yan</surname>
<given-names>B.</given-names>
</name>
<name>
<surname>Hua</surname>
<given-names>T.</given-names>
</name>
<name>
<surname>Fuqian</surname>
<given-names>J.</given-names>
</name>
</person-group> (<year>2002</year>). <article-title>Electrical Conductivity of Iron under Shock Compression up to 200 GPa</article-title>. <source>J. Phys. Cond. Matter</source> <volume>14</volume>, <fpage>10849</fpage>. <pub-id pub-id-type="doi">10.1088/0953-8984/14/44/389</pub-id> </citation>
</ref>
<ref id="B35">
<citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname>Yokoo</surname>
<given-names>S.</given-names>
</name>
<name>
<surname>Hirose</surname>
<given-names>K.</given-names>
</name>
<name>
<surname>Sinmyo</surname>
<given-names>R.</given-names>
</name>
<name>
<surname>Tagawa</surname>
<given-names>S.</given-names>
</name>
</person-group> (<year>2019</year>). <article-title>Melting Experiments on Liquidus Phase Relations in the Fe&#x2013;S&#x2013;O Ternary System under Core Pressures</article-title>. <source>Geophys. Res. Lett.</source> <volume>46</volume>, <fpage>5137</fpage>&#x2013;<lpage>5145</lpage>. <pub-id pub-id-type="doi">10.1029/2019gl082277</pub-id> </citation>
</ref>
</ref-list>
</back>
</article>