高温高压下碳酸盐和含水矿物电导率研究任务书

 2021-10-25 09:10

1. 毕业设计(论文)的内容和要求

通过开展极端条件下地球与行星内部物质物理和化学性质的研究,进而探索太阳系天体内部运行机制和早期演化历史。

极端条件,包括高温、高压、强辐射和冲击等,将会极大地改变地球与行星物质的物理性质和化学行为。

通过高温、高压等实验技术模拟地球与行星内部极端环境,并且与理论计算、数值模拟等方面的工作相结合,系统深入地研究探讨地球和行星内部如何运行。

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2. 参考文献

根据毕业要求指点2.3和10.2,参考文献如下:[1] Lin J F , Liu J , Jacobs C , et al. Vibrational and elastic properties of ferromagnesite across the electronic spin-pairing transition of iron[J]. American Mineralogist, 2012, 97(4):583-591.[2] Chengwei Zhang,Jung‐Fu Lin,Ying Liu,Shaomin Feng,Changqing Jin,Mingqiang Hou,Takashi Yoshino. Electrical Resistivity of Fe‐C Alloy at High Pressure: Effects of Carbon as a Light Element on the Thermal Conductivity of the Earth's Core[J]. Journal of Geophysical Research. Solid Earth,2018, 123(5).[3]田浩然,2019,高压下单晶橄榄石的电导率,高压物理学报。

[4]K. Ohta et al., Experimental and theoretical evidence for pressure-induced metallization in FeO with rocksalt-type structure. Phys. Rev. Lett. 108, 026403 (2012).[5]K. Ohta, et al., The electrical conductivity of post-perovskite in Earth's D''layer. Science 320, 89-91 (2008).[6]J.F. Lin et al., Effects of the electronic spin transitions of iron in lower mantle minerals: Implications for deep mantle geophysics and geochemistry, Reviews of Geophysics 51, 244-275 (2013).[7]J. Liu, et al.Hydrogen-bearing iron peroxide and the origin of ultralow-velocity zones. Nature 551, 494 (2017).[8]Plank 352 (2019).[9] T. Yoshino, T. Katsura, Electrical conductivity of mantle minerals: Role of water in conductivity anomalies. Annu. Rev. Earth Planet. Sci. 41, 605628 (2013).[10] T. Yoshino, T. Katsura, Electrical conductivity of mantle minerals: Role of water in conductivity anomalies. Annu. Rev. Earth Planet. Sci. 41, 605628 (2013).

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