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The parameterization of solid metal-liquid metal partitioning of siderophile elements

机译:嗜铁元素的固-液-金属分配参数化

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摘要

Many solar system processes involve a metallic liquid, and the composition of the metallic liquid, such as the liquid's concentrations of S, P, and C, will influence the partitioning of elements during such processes. We present a method for parameterizing solid metal-liquid metal partition coefficients for siderophile (metal-loving) elements as a function of the metallic liquid composition. Our parameterization method is based on an older theory of Jones and Malvin (1990), which stated that the metallic liquid is composed of metal and non-metal-bearing domains, and the domains are the dominant influence on the partitioning behavior. By revising the means by which the metal domains are calculated. our revised parameterization method is able to match experimental partitioning data from the Fe-Ni-S, Fe-Ni-S-P, and Fe-Ni-C systems. Mathematical expressions were derived for the solid metal-liquid metal partitioning of 13 siderophile elements. Elements that are chalcophile (S-loving), P-loving, or C-loving prefer the non-metal-bearing domains in the metallic liquid and, consequently, aren't fit by the parameterization method presented here, Possible applications for our parameterization method include modeling the crystallization of iron meteorites, planetary differentation, and the solidification of Earth's inner core.
机译:许多太阳系过程都涉及金属液体,金属液体的组成(例如液体中S,P和C的浓度)将影响此类过程中元素的分配。我们提出了一种参数化方法,用于根据金属液体成分来参数化嗜铁(嗜金属)元素的固体金属-液体金属分配系数。我们的参数化方法基于琼斯和马尔文(Jones and Malvin,1990)的较旧理论,该理论指出金属液体是由金属和非金属域组成的,并且域是对分配行为的主要影响。通过修改计算金属域的方法。我们修改后的参数化方法能够匹配来自Fe-Ni-S,Fe-Ni-S-P和Fe-Ni-C系统的实验分区数据。推导了13种嗜铁元素的固-液-金属分配的数学表达式。嗜硫(喜欢S),喜欢P或喜欢C的元素更喜欢金属液体中的非金属域,因此不适合此处介绍的参数化方法,我们的参数化可能应用方法包括模拟铁陨石的结晶,行星的差异和地球内核的凝固。

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