2018
DOI: 10.1029/2018jb015522
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Ab Initio Prediction of Potassium Partitioning Into Earth's Core

Abstract: Potassium partitioning between molten silicates and liquid iron alloys is the fundamental process determining its incorporation into the Earth's core. In this study, it is investigated using the method of the ab initio molecular dynamics simulation combined with the thermodynamic integration technique. Results suggest that the potassium incorporation into iron alloys positively depends on temperature, while the effect of pressure is insignificant. Moreover, the existence of oxygen in liquid iron alloys signifi… Show more

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Cited by 21 publications
(25 citation statements)
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References 45 publications
(87 reference statements)
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“…Temperature is generally considered to be an essential factor affecting the partitioning behavior of elements (e.g., Chabot et al., 2005; Righter, 2011; Xiong et al., 2018), while the simulations in this work were conducted at a constant temperature of 5,000 K. Here, we extrapolated the metal/silicate partition coefficients of He and Ar to lower temperatures based on the Boltzmann relation (Text ). The results show that D He and D Ar decrease by approximately one order of magnitude (Figure ) as temperature decreases from 5,000 to 3,500 K. On the other hand, the density of the outer core is ∼10% lighter than pure liquid Fe, due to the presence of light elements( x ) such as H, C, O, S, Si, etc.…”
Section: Resultsmentioning
confidence: 99%
“…Temperature is generally considered to be an essential factor affecting the partitioning behavior of elements (e.g., Chabot et al., 2005; Righter, 2011; Xiong et al., 2018), while the simulations in this work were conducted at a constant temperature of 5,000 K. Here, we extrapolated the metal/silicate partition coefficients of He and Ar to lower temperatures based on the Boltzmann relation (Text ). The results show that D He and D Ar decrease by approximately one order of magnitude (Figure ) as temperature decreases from 5,000 to 3,500 K. On the other hand, the density of the outer core is ∼10% lighter than pure liquid Fe, due to the presence of light elements( x ) such as H, C, O, S, Si, etc.…”
Section: Resultsmentioning
confidence: 99%
“…DFT‐MD simulations give potential energy ( U ) and pressure ( P ) but not entropy ( S ) of the system; combining DFT‐MD with the thermodynamic integration method provides a general scheme for computing the Helmholtz energy ( F ) difference Δ F = F B – F A of two systems containing the same number of atoms which are governed by different potential energy functions U B (target system) and U A (reference system) (e.g., Alfè et al, 2000; Vočadlo et al, 2008; Wahl & Militzer, 2015; Xiong et al, 2018). For the metal and silicate liquids considered in this study, we use the ideal gas as reference, for which F can be calculated analytically.…”
Section: Computational Detailsmentioning
confidence: 99%
“…to enable positive E J before inner core formation. The drawback here is that experiments and simulations suggest that little 40 K partitioned into the core during formation (Chidester et al, 2017;Xiong et al, 2018). Precipitation provides another potential solution, though as we have seen it introduces a number of uncertain parameters and is difficult to constrain from available observations (though see Helffrich et al, 2018).…”
Section: Towards Resolving the New Core Paradoxmentioning
confidence: 92%
“…below. We have also neglected radiogenic heating since potassium 40 is not thought to partition significantly into the core (Xiong et al, 2018). In this section we also ignore Q p and E p , but will reintroduce them when considering precipitation in Section 5.…”
Section: Evolution Of Thermal Stratificationmentioning
confidence: 99%
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