Collaborative Research: Experimental Determination of Iron (Fe) Isotope Fractionations in Sulfide Minerals

知识价值。铁（Fe）同位素地球化学领域发展迅速，目前世界上20多个研究小组的75多篇论文中包含数千种同位素分析。这些工作大多集中在自然系统上，只有少数实验确定的动力学和平衡分馏因子以及相关的交换动力学数据可用于地质相关系统。地球上铁同位素组成的最大变化记录在硫化物中，在沉积黄铁矿中发现了56Fe/54Fe比例的近5 permil范围，在高温热液硫化物中发现了3 permil范围，但在水和矿物Fe- s系统中，铁同位素分馏机制尚不清楚。一个全面的实验计划，以确定铁同位素在水Fe- s物种和硫化物矿物之间的分馏，温度范围高达~250℃。实验计划将探索三个系统中的同位素分馏，涵盖一些最常见的水和矿物物种。动力学和平衡铁同位素分馏将被研究，包括探索不同的硫化物形成途径及其相关的同位素交换动力学，这些问题可能在确定硫化物矿物的铁同位素组成中起主要作用。除温度外，我们还将探讨pH和微量金属取代对Fe同位素分馏和交换动力学的影响。更广泛的影响。硫化物的铁同位素地球化学已被用于研究从生命的起源和演化到热液矿床中金属的来源等问题。本研究产生的同位素分馏机制的可用性将加强对这些数据的解释。此外，将采用新的实验方法，这些方法将普遍适用于矿物合成的其他实验研究。该研究团队融合了来自三个机构的同位素和实验地球化学的基本专业知识。该项目将资助和培养三所院校的几名研究生和一名博士后。其中包括一名来自加纳的博士生和一名来自乌拉圭的女博士后科学家。此外，这项研究将涉及一位早期职业助理教授。

Intellectual Merit. The field of Iron (Fe) isotope geochemistry has grown rapidly and the literature now contains several thousand isotopic analyses in over 75 papers from two-dozen research groups in the world. Most of this work has focused on natural systems, and only a handful of experimentally determined kinetic and equilibrium fractionation factors and associated exchange kinetic data are available for geologically relevant systems. The largest variations in Fe isotope compositions on Earth are recorded in sulfides, where almost a 5 permil range in 56Fe/54Fe ratios is found in sedimentary pyrite and a 3 permil range in high-temperature hydrothermal sulfides, and yet Fe isotope fractionation mechanisms in aqueous and mineral Fe-S systems poorly known. A comprehensive experimental program is planned for determining the Fe isotope fractionations among aqueous Fe-S species and sulfide minerals over the temperature range up to ~250 C. The experimental program will explore isotopic fractionations in three systems covering some of the most common aqueous and mineral species. Both kinetic and equilibrium Fe isotope fractionations will be investigated, including exploration of different sulfide formation pathways and their associated isotopic exchange kinetics, issues that may play a major role in determining the Fe isotope compositions of sulfide minerals. In addition to temperature, we will explore the effects of pH and trace metal substitution on Fe isotope fractionation and exchange kinetics.Broader Impacts. Iron isotope geochemistry of sulfides has been used to investigate problems ranging from the origin and evolution of life to the sources of metals in hydrothermal ore deposits. Interpretations of these data will be enhanced by availability of isotopic fractionation mechanisms generated by this study. In addition, new experimental approaches will be employed that will be generally applicable to other experimental studies of mineral synthesis. The research team blends essential expertise in isotope and experimental geochemistry from three institutions. The project will support and educate several graduate students and a post-doc from the three institutions. These include a Ph.D. student from Ghana and a female post-doctoral scientist from Uruguay. In addition, the research will involve an early-career Assistant Professor.