姓名:严薇

职称:助理研究员
邮件:yanwei@sio.org.cn
通讯地址:浙江省杭州市西湖区保俶北路36号
专业:地球化学
研究方向:

实验地球化学、海底资源与成矿系统

个人简介:

2022.9-至今:自然资源部第二海洋研究所,助理研究员

2018.9-2022.6:北京大学地球与空间科学学院,地球化学,理学博士学位

2015.9-2018.7:中国地质大学(北京)珠宝学院,宝石学,理学硕士学位

2011.9-2015.7:中国地质大学(北京)珠宝学院,宝石及材料工艺学,工学学士学位


承担项目:
科研成果:

已公开发表学术论文11篇(截至2022年9月)。其中,以第一作者发表SCI论文3篇,中文核心论文1篇。

[1] Yan W, Lv M, He M, Liu X (2022). Effect of second Si-O vibrational overtones/combinations on quantifying water in silicate and silica minerals using infrared spectroscopy, and an experimental method for its removal. Physics and Chemistry of Minerals 49, 5. 

[2] Yan W, Zhang Y, Ma Y, He M, Zhang L, Sun W, Wang CY, Liu X (2021). Water in coesite: Incorporation mechanism and operation condition, solubility and P-T dependence, and contribution to water transport and coesite preservation. Geoscience Frontiers 12, 313-326.

[3] Yan W, Liu X, Sun S, Sun W, Wu D (2021). Experimental constraints on trace element partitioning between coesite and hydrous silicate melt at 5 GPa and 1500-1750 °C. SCIENCE CHINA Earth Sciences 64, 1171-1183. 严薇, 刘曦, 孙赛军, 孙卫东, 吴丹 (2021). 5GPa、1500∼1750 °C条件下微量元素在柯石英与含水硅酸盐熔体之间分配行为的实验研究. 中国科学: 地球科学 51, 1375-1388.

[4] 严薇, 刘曦 (2021). 名义上无水矿物中水的定量方法及其优缺点:重点讨论FTIR方法与其存在问题. 矿物岩石地球化学通报 40, 425-447.

[5] Ma Y, Yan W, Sun Q, Liu X (2021). Raman and infrared spectroscopic quantification of the carbonate concentration in K2CO3 aqueous solutions with water as an internal standard. Geoscience Frontiers 12, 1018-1030.

[6] He M, Yan W, Chang Y, Liu K, Liu X (2019). Fundamental infrared absorption features of α-quartz: An unpolarized single-crystal absorption infrared spectroscopic study. Vibrational Spectroscopy 101, 52-63.

[7] Wang B, Zhang Y, Fu S, Yan W, Takahashi E, Li L, Lin J-F, Song M (2022). Single-crystal elasticity of phase Egg AlSiO3OH and δ-AlOOH by Brillouin spectroscopy. American Mineralogist, 107, 147-152.

[8] Wang Y, He M, Yan W, Yang M, Liu X (2020). Jianite: massive dunite solely made of virtually pure forsterite from Ji’an County, Jilin Province, Northeast China. Minerals 10, 220.

[9] Liu L, Ma Y, Yan W, Liu X (2019). Trace element partitioning between MgAl2O4-spinel and carbonatitic silicate melt from 3 to 6 GPa, with emphasis on the role of cation order-disorder. Solid Earth Sciences 4, 43-65.

[10] Liu X, Sui Z, Fei H, Yan W, Ma Y, Ye Y (2020). IR features of hydrous Mg2SiO4-ringwoodite, unannealed and annealed at 200-600 °C and 1 atm, with implications to hydrogen defects and water-coupled cation disorder. Minerals 10, 499.

[11] Liu L, Liu X, Bao X, He Q, Yan W, Ma Y, He M, Tao R, Zou R (2018). Si-disordering in MgAl2O4-spinel at high P-T conditions, with implications to Si-Mg disorder in Mg2SiO4-ringwoodite. Minerals 8, 210.