个人简历
“地大百人”特聘教授。2019 年获日本东北大学博士学位,2019–2023 年在拜仁地质研究所从事博士后研究。
荣获“国家级人才项目”、“楚天学者”、“地大百人”等。曾主持:① 德国“洪堡学者”基金、② 德国科学基金会(DFG)基金。
研究方向
地球深部物质的物理化学性质,内容涵盖:(1)元素分配;(2)同位素分馏;(3)矿物相变;(4)弹性与地震波速等。
研究方法包括:第一性原理计算(如 VASP)、分子动力学模拟(如 LAMMPS),以及高温高压实验(如大腔体压机、金刚石压砧)。

图:课题组超算,含 21 个计算节点/2688 个物理核心(其中 8 个为 CPU+GPU 节点,含16 块 RTX 4090 显卡)
第一/通讯作者论文
[9] Zhang, P., Man, L., Yuan, L.*, Wu, X., Zhang, J., 2025. Ultra-low-velocity disordered CaCO3 may explain mid-lithospheric discontinuities. Journal of Geophysical Research: Solid Earth, 130(9), e2025JB031906. https://doi.org/10.1029/2025JB031906 (Editors' Highlights)
[8] Yuan, L.*, Steinle‐Neumann, G., 2024. Earth's "missing" chlorine may be in the core. Journal of Geophysical Research: Solid Earth, 129, e2023JB027731. https://doi.org/10.1029/2023JB027731
[7] Yuan, L.*, Steinle-Neumann, G., 2023. Hydrogen distribution between the Earth's inner and outer core. Earth and Planetary Science Letters, 609, 118084. https://doi.org/10.1016/j.epsl.2023.118084
[6] Yuan, L.*, Steinle‐Neumann, G., 2022. Possible control of Earth's boron budget by metallic iron. Geophysical Research Letters, 49, e2021GL096923. https://doi.org/10.1029/2021GL096923
[5] Yuan, L.*, Steinle‐Neumann, G., 2021. The helium elemental and isotopic compositions of the Earth's core based on ab initio simulations. Journal of Geophysical Research: Solid Earth, 126, e2021JB023106. https://doi.org/10.1029/2021jb023106
[4] Yuan, L.*, Steinle-Neumann, G., 2020. Strong sequestration of hydrogen into the Earth's core during planetary differentiation. Geophysical Research Letters, 47, e2020GL088303. https://doi.org/10.1029/2020GL088303
[3] Yuan, L.*, Steinle‐Neumann, G., Suzuki, A., 2020. Structure and density of H2O‐rich Mg2SiO4 melts at high pressure from ab initio simulations. Journal of Geophysical Research: Solid Earth, 125, e2020JB020365. https://doi.org/10.1029/2020JB020365
[2] Yuan, L.*, Ohtani, E., Ikuta, D., Kamada, S., Tsuchiya, J., Naohisa, H., Ohishi, Y., Suzuki, A., 2018. Chemical reactions between Fe and H2O up to megabar pressures and implications for water storage in the Earth's mantle and core. Geophysical Research Letters, 45, 1330–1338. https://doi.org/10.1002/2017GL075720
[1] Yuan, L.*, Ohtani, E., Shibazaki, Y., Ozawa, S., Jin, Z., Suzuki, A., Frost, D.J., 2018. The stability of anhydrous phase B, Mg14Si5O24, at mantle transition zone conditions. Physics and Chemistry of Minerals, 45, 523–531. https://doi.org/10.1007/s00269-017-0939-5
合作论文
[7] Aslandukova, A., Aslandukov, A., Yuan, L., Laniel, D., Khandarkhaeva, S., Fedotenko, T., Steinle-Neumann, G., Glazyrin, K., Dubrovinskaia, N., Dubrovinsky, L., 2021. Novel high-pressure yttrium carbide γ − Y4C5 containing [C2] and nonlinear [C3] units with unusually large formal charges. Physical Review Letters 127, 135501. https://doi.org/10.1103/physrevlett.127.135501
[6] Aslandukov, A., Aslandukova, A., Laniel, D., Koemets, I., Fedotenko, T., Yuan, L., Steinle-Neumann, G., Glazyrin, K., Hanfland, M., Dubrovinsky, L., Dubrovinskaia, N., 2021. High-pressure yttrium nitride, Y5N14, featuring three distinct types of nitrogen dimers. Journal of Physical Chemistry C 125, 18077–18084. https://doi.org/10.1021/acs.jpcc.1c06210
[5] Koemets, E., Yuan, L., Bykova, E., Glazyrin, K., Ohtani, E., Dubrovinsky, L., 2020. Interaction between FeOOH and NaCl at extreme conditions: synthesis of novel Na2FeCl4OHx compound. Minerals 10, 51. https://doi.org/10.3390/min10010051
[4] Ishii, T., Huang, R., Myhill, R., Fei, H., Koemets, I., Liu, Z., Maeda, F., Yuan, L., Wang, L., Druzhbin, D., Yamamoto, T., Bhat, S., Farla, R., Kawazoe, T., Tsujino, N., Kulik, E., Higo, Y., Tange, Y., Katsura, T., 2019. Sharp 660-km discontinuity controlled by extremely narrow binary post-spinel transition. Nature Geoscience 12, 869–872. https://doi.org/10.1038/s41561-019-0452-1
[3] Ikuta, D., Ohtani, E., Sano-Furukawa, A., Shibazaki, Y., Terasaki, H., Yuan, L., Hattori, T., 2019. Interstitial hydrogen atoms in face-centered cubic iron in the Earth's core. Scientific Reports 9, 7108. https://doi.org/10.1038/s41598-019-43601-z
[2] Ishii, T., Huang, R., Fei, H., Koemets, I., Liu, Z., Maeda, F., Yuan, L., Wang, L., Druzhbin, D., Yamamoto, T., Bhat, S., Farla, R., Kawazoe, T., Tsujino, N., Kulik, E., Higo, Y., Tange, Y., Katsura, T., 2018. Complete agreement of the post-spinel transition with the 660-km seismic discontinuity. Scientific Reports 8, 6358. https://doi.org/10.1038/s41598-018-24832-y
[1] Ohtani, E., Yuan, L., Ohira, I., Shatskiy, A., Litasov, K., 2018. Fate of water transported into the deep mantle by slab subduction. Journal of Asian Earth Sciences 167, 2–10. https://doi.org/10.1016/j.jseaes.2018.04.024
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