CAREER: Experimental Constraints on Carbon-iron Redox Interaction in Earth's Deep Lower Mantle

地球的深层碳循环影响着地球上生命的过去、现在和未来。深层的碳化学是碳固存和火山活动的原因。钻石在深处的生长不仅推动了一个行业，而且还捕获和保存了我们唯一的地球深部样品。下地幔是地球最大的一层，即使浓度很低，也有很大的碳容量，因此对全球碳预算很重要。该项目将把地幔在地球深层碳循环中的作用的研究与一项教育计划结合起来，该计划包括在密歇根州立大学及其他地方招募不同的学生参加实验室地球科学，并改善空间推理教学，这是地球科学家的一项关键技能。整个地球的碳循环是一个非常适合推广的及时主题，以吸引对环境问题感兴趣的学生从事地球科学职业。将为密歇根州立大学地质学和全球变化入门课程开发碳矿物学和地球化学短模块。这些练习的有效性将在本科专业的招聘和发展空间推理技能的地球科学职业方面进行评估。本科生和研究生研究助理将参与实验室和地球科学教学评估。主要研究目标是确定下地幔条件下岩石学背景下含碳相的稳定性。地幔矿物学和氧逸度（fO 2）的深度和区域依赖性差异将导致地幔相组合中碳的形态和宿主相的变化。量化含碳相的稳定性与压力、温度、氧化还原条件和主要矿物学之间的关系，对于了解地球内部碳的命运至关重要。在激光加热的金刚石对顶砧单元进行的实验将提供一些第一个实验约束碳酸盐和碳化物的稳定性和物理性质的岩石学背景下的地幔相组合在压力-温度条件下达到核幔边界（CMB）。这些实验的结果将有助于地球化学家、宇宙化学家、火山学家、岩石学家、矿物学家和地球化学家对碳的起源、储存和通量有一个全面的了解。地球的碳循环和大众对钻石的兴趣提供了一个通过课程和研究助学金教学和招生的机会。该项目的教育部分是PI和地理认知专家Julie Libarkin博士之间的合作，以开发和评估包含深层碳背景和开发3D推理技能的教育模块。该奖项反映了NSF的法定使命，并被认为是值得通过使用基金会的知识价值和更广泛的影响审查标准进行评估的支持。

Earth's deep carbon cycle affects the past, present and future of life on our planet. Carbon chemistry at depth is responsible for carbon sequestration and volcanism. The growth of diamonds at depth not only drives an industry, but also traps and preserves our only samples of Earth's deep interior. Earth's lower mantle, the Earth's biggest layer, has great capacity for carbon even at very low concentrations and is thus important to the global carbon budget. The project will integrate research in the role of the mantle in Earth's deep carbon cycle with an education plan that includes recruitment of diverse students to laboratory geoscience and improves teaching of spatial reasoning, a critical skill for Earth scientists, at Michigan State University (MSU) and beyond. The whole-Earth carbon cycle is a timely subject well-suited to outreach to attract students with interest in environmental problems to careers in geosciences. Short modules on carbon mineralogy and geochemistry will be developed for gateway courses in geology and global change at MSU. The effectiveness of these exercises will be assessed in terms of recruitment of undergraduate majors and developing spatial reasoning skills for geoscience careers. Undergraduate and graduate research assistants will participate both in the lab and in geoscience teaching evaluation.The primary research goal is to determine the stability of carbon-bearing phases in petrologic context at conditions of the lower mantle. Depth- and region-dependent differences in mantle mineralogy and oxygen fugacity (fO2) will result in changes in the speciation and host phases of carbon within the mantle phase assemblage. Quantifying the relationship between stability of carbon-bearing phases and pressure, temperature, redox conditions, and major mineralogy is critical to understanding the fate of carbon in Earth's interior. Experiments performed in laser-heated diamond anvil cells will provide some of the first experimental constraints on carbonate and carbide stability and physical properties in petrologic context of mantle phase assemblages at pressure-temperature conditions reaching the Core-Mantle Boundary (CMB). The results of the proposed experiments will be necessary to an integrated understanding of the origin, storage, and flux of carbon among a community including geochemists, cosmochemists, volcanologists, petrologists, mineralogists, and geophysicists. Earth's carbon cycle and popular interest in diamonds offer an opportunity to teach and recruit students through coursework and research assistantships. The education component of this project is a collaboration between the PI and geocognition expert Dr. Julie Libarkin to develop and evaluate educational modules incorporating deep carbon context and developing 3D reasoning skills. Modules will be evaluated by in-class observations, surveys and interviews and disseminated openly online.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.