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中国科技大学地球和空间科学学院导师教师师资介绍简介-郝记华

本站小编 Free考研考试/2021-04-24

邮箱: hao@ustc.edu.cn




个人简介
郝记华,男,1991年生于山东省莘县。中国科学技术大学地球和空间科学学院特任研究员。研究方向包括地球早期表生化学循环,生命起源和演化,高温高压水-岩反应,地球和行星条件下光化学,太阳系冰卫星海水化学等。

学习经历
2012年8月-2016年11月 约翰霍普金斯大学(JHU),地球与行星科学系,地球化学,硕士及博士。
2008年8月-2012年七月 中国科学技术大学,地球与空间科学学院,环境科学,学士。

工作经历
2021年1月-今,中国科学技术大学,地球与空间科学学院,特任研究员
2019年9月-2020年12月,美国罗格斯大学,海洋与近海科学系,博士后
2016年12月-2019年8月,法国里昂一大,地质系,博士后


发表文章
Hao*, J.,Knoll, A.H., Fang, H., Schieber, J., Hazen, R.M., Daniel, I. (2020) Cycling ofphosphorus on the Archean Earth: Part II. Phosphorus Limitation on PrimaryProduction in Archean Ecosystems. Geochimica et Cosmochimica Acta, 280,360-377.
Hao*,J., Knoll, A.H., Fang, H., Hazen, R.M., Daniel, I. (2020)Cycling of phosphorus on the Archean Earth: Part I. Continental weathering andriverine transport of phosphorus. Geochimica et Cosmochimica Acta, 273, 70-84.
Moore#,E.K., Hao#, J., Spielman, S.J., Yee, N. (2020) The Evolving RedoxChemistry and Bioavailability of Vanadium in Deep Time (*co-first author).Geobiology 18(2), 127-138. (#共同第一作者)
Hao*,J., Sverjensky, D.A., and Hazen, R.M. (2019) Redox states ofArchean surficial environments: the importance of H2,g instead of O2,g forweathering reactions. Chemical Geology, 521, 49-58.
Hao*,J., Mokhtari, M., Pedreira-Segade, U., Michot, L.M., andDaniel#, I. (2019) Transition metals enhance the adsorption of nucleotides ontoclay: implications for the origin of life. ACS Earth and Space Chemistry, 3(1),109-119.
Hao*,J., Giovenco, E., Pedreira-Segade, U., Montagnac, G., Daniel,I. (2018) Compatibility of amino acids in ice Ih: implications for the originof life. Astrobiology, 18, 381-392. Featured and cover article
Hao*,J., Sverjensky, D.A., and Hazen, R.M. (2017) Mobility of nutrientsand trace elements during weathering on the Archean. Earth and PlanetaryScience Letters, 478, 148-159.
Hao*, J.,Sverjensky, D.A. and Hazen, R.M. (2017) A model for late Archean chemicalweathering and world average river water. Earth and Planetary Science Letters,457, 191-203.
Tang,M., Chu, X., Hao, J., Shen, B. Orogenic quiescence in Earth’s middleage. Science (in press)
Montagnac,G., Hao, J., Pedreira-Segade, U., Daniel, I. (2021) Detection ofnucleotides absorbed onto clay by UV Resonant Raman Spectroscopy: a steptowards the search for biosignatures on Mars. Applied Clay Science, 200,105824.
Huang,F., Barbier, S., Tao, R., Hao, J., and others. (2020) Dataset for H2,CH4 and organic compounds formation during experimental serpentinization.Geoscience Data Journal.
Liu,W., Hao, J., Yee, N., Elzinga, E.J., Piotrowiak, P., Nanda, V.,Falkowski, P. (2020) Anoxic photogeochemical oxidation of manganese carbonateyields manganese oxide. Proceedings of National Academy of Sciences. USA 117(37).
周强,姜允斌,郝记华,季峻峰,李伟#(2020) 磷的生物地球化学循环研究进展, 高校地质学报 (已接收)
Huang#,F., Barbier, S., Tao, R., Hao, J., et al. (2020) A review of H2, CH4 andhydrocarbon formation in experimental serpentinization using network analysis,Frontiers in Earth Science 8
Mignon#,P., Corbin, G., Le Crom, S., Marry, V., Hao, J., Daniel, I. (2020)Adsorption of Nucleotides on Clay Surfaces. Effects of mineral composition, pHand solution salts. Applied Clay Science, 190, 105544.
Huang#,J., Hao, J., Huang, F., Sverjensky, D. (2019) Mobility of chromium inhigh-temperature crustal and upper mantle fluids. Geochemical PerspectivesLetters 12, 1-6.
Pedreira-Segade#,U., Hao, J., Montagnac, G., Cardon, H., Daniel, I. (2019) Spontaneouspolymerization of glycine under hydrothermal conditions. ACS Earth and SpaceChemistry, 3(8), 1669-1677.
Pedreira-Segade,U., Hao, J., Razafitianamaharavo, A., Pelletier, M., Marry, V., Le Crom,S., Michot, L., Daniel#, I. (2018) How do nucleotides adsorb onto clays? Life,8(4), 59.
Moore#,E.K., Hao, J., Prabhu, A., Zhong, H., Jelen, B.I., Meyer, M., Hazen,R.M., Falkowski, P.G. (2018) Geological and chemical factors that impacted thebiological utilization of cobalt in the Archean era. Journal of GeophysicalResearch: Biogeosciences, 123, 743-759.
Estrada#,C.F., Mamajov, I., Hao, J., Sverjensky, D.A., Cody, G.D., Hazen, R.M.(2017) Aspartate transformation at 200 °C with brucite [Mg(OH)2], NH3, and H2:implications for prebiotic molecules in hydrothermal systems. Chemical Geology,457, 162-172. Invited research article






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