Hadal Science and Technology Research Center

The deep science and technology project was inspired by the "dragon". The jiaolong sea trials at level 5000 m and 5000 m level invited during sea trials Please try the Marine scientists involved in the sea process, fully tap the latent time the scientific value of each test, let volunteers engineers realized the benefits of scientists and engineers are closely combined. , on the other hand, from the United States in 2010 to commemorate the human in order to the marianas trench Deep - "challenger deep" writing in the 50th anniversary of the memorial of awareness of the deep science and technology is the forefront of science and technology in the field of ocean. Therefore ...More+

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science team

Min LUO

Jobs:
Position:
Research:
Email: luomin@gig.ac.cn

Education:
2006.9-2010.6Shandong University of Science and Technology, B.Sc. (Geology)
2010.9-2015.6                Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Ph.D.
(Geochemistry)
2013.10-2015.1              GEOMAR, joint-training PhD candidate (Biogeochemical modeling in cold     
seeps)
 
Professional Experience:
2016.3-                          Research Assistant, Hadal Science and Technology Research Center, Shanghai
Ocean University
2015.7-2016.2               Research Assistant, Guangzhou Institute of Geochemistry, Chinese Academy
of Sciences
 
Current Research Interests:
-Fluid flow and water-rock reactions in serpentinization mud volcanoes
- Modeling of organic matter degradation in hadal trench sediments
- Carbon and sulfur cycles in cold seeps
 
Publications:
1.      Luo, M., Dale, A.W., Wallmann, K., Hensen, C., Gieskes, J., Yan, W., Chen, D., 2015. Estimating the time of pockmark formation in the SW Xisha Uplift (South China Sea) using reaction-transport modeling. Marine Geology 364, 21-31.
2.      Luo, M., Chen, L., Tong, H., Yan, W., Chen, D., 2014. Gas hydrate occurrence inferred from dissolved Cl− concentrations and δ18O values of pore water and dissolved sulfate in the shallow sediments of the pockmark field in southwestern Xisha Uplift, northern South China Sea. Energies 7, 3886-3899.
3.      Luo, M., Huang, H., Zhang, P., Wu, Q., Chen, D., 2014. Origins of gas discharging from the Qiangtang Basin in the northern Qinghai–Tibet Plateau, China: Evidence from gas compositions, helium, and carbon isotopes. Journal of Geochemical Exploration146, 119-126.
4.      Luo, M., Chen, L., Wang, S., Yan, W., Wang, H., Chen, D., 2013. Pockmark activity inferred from pore water geochemistry in shallow sediments of the pockmark field in southwestern Xisha Uplift, northwestern South China Sea. Marine and Petroleum Geology 48, 247-259.
 
Conference Proceedings:
1.      Luo, M., Dale, A., Wallmann, K., Chen, D. Microbial turnover and benthic geochemical flux of the pockmark field in southwestern Xisha Uplift, northern South China Sea: Insight from reaction-transport model. 12th International Conference on Gas in Marine Sediments (GIMS12), 2014, Taiwan.
2.      Luo, M., and Chen, D. Benthic fluxes of methane and dissolved inorganic carbon of the pockmark field in southwestern Xisha Uplift, northwestern South China Sea: A numerical modelling perspective. Goldschmidt Conference, 2014, Sacramento, USA.
3.      Luo, M., Huang, H., Zhang, P., Wu, Q., Chen, D. Gas types and origins inferredfromthe geochemistry of seeping gases in the Qinghai-Tibet Plateau, China. ICGG-12, 2013, Greece.