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Name: Yongsheng Huang

Title: Associate researcher

Phone: ----

Email: huangyongsheng@gig.ac.cn; mountainandspring@163.com

 

Resume:

2021.11-now. Associate researcher. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences.

2020.04–2021.10. Postdoctoral researcher, Tohoku University, Japan.

2016.10–2020.03. Ph.D., Joint Doctoral Program operated by Tohoku University and Bayerisches Geoinstitut (BGI), University of Bayreuth.

2013.09–2016.07. Master, Institute of Geochemistry, University of Chinese Academy of Sciences, China.

2009.09–2013.07. Bachelor, Kunming University of Science and Technology, China.


Research Interests:

Geological Fluid/Volatile Cycle

High-temperature and high-pressure experiments simulate the physic-chemical conditions within the Earth, studying the distribution characteristics and migration mechanisms of fluids/melts in the Earth's interior, exploring the geochemical behavior of elements during the interaction between deep rocks and fluids/melts.

Simulation Study on Planetary Surface Evolution

Experimental simulations of the physic-chemical conditions on and near planetary surfaces investigate the effect of rock-fluid interactions under extreme planetary conditions on the composition of planetary surfaces and atmospheres.

Physical Properties of Rocks under Extreme Conditions

In-situ rock conductivity measurements under high-temperature and high-pressure conditions, combined with synchrotron radiation X-ray tomography, provide experimental constraints for the causes of geophysical anomalies, revealing differences in material composition, structure, and tectonics across different planetary layers.

The Influence of Differential Stress

Deformation experiments under high-temperature and high-pressure conditions explore the effects of differential stress on the physic-chemical properties of deep rocks.


Recent Publications:

Huang Y.*, Okumura S., Matsumoto K., Takahashi N., Tang H., Wu G., Tsujimori T., Nakamura M., Okamoto A., Li Y. 2024. Experimental constraints on serpentinite carbonation in the presence of a H2O–CO2–NaCl fluid. Contributions to Mineralogy and Petrology 179(11): 98. https://doi.org/10.1007/s00410-024-02175-4

Huang, Y.*, Nakatani, T., Sawa S., Wu, G., Nakamura, M., McCammon, C. 2023. Effect of faceting on olivine wetting properties. American Mineralogist 108(12): 2244–59. https://doi.org/10.2138/am-2022-8808

Huang, Y.*, Guo, H., Nakatani, T., Uesugi, K., Nakamura, M., Keppler, H. 2021. Electrical conductivity in texturally equilibrated fluid-bearing forsterite aggregates at 800°C and 1 GPa: Implications for the high electrical conductivity anomalies in mantle wedges. Journal of Geophysical Research: Solid Earth 126, e2020JB021343. https://doi.org/10.1029/2020JB021343

Huang, Y.*, Nakatani, T., Nakamura, M., McCammon, C. 2020. Experimental constraint on grain-scale fluid connectivity in subduction zones. Earth and Planetary Science Letters 552, 116610. https://doi.org/10.1016/j.epsl.2020.116610

Huang, Y.*, Nakatani, T., Nakamura, M., McCammon, C. 2019. Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties. Nature Communications 10, 5557. https://doi.org/10.1038/s41467-019-13513-7

黄永胜, 张辉, 吕正航, 唐勇, 唐宏, 2016. 新疆阿尔泰二叠纪, 三叠纪伟晶岩侵位深度研究: 来自流体包裹体的指示. 矿物学报, 36(4), 571-585. https://doi.org/10.16461/j.cnki.1000-4734.2016.04.018

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