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分类:导师信息 来源:中国考研网 2015-07-25 相关院校:兰州大学
姓 名 | 管清玉 | ||
---|---|---|---|
性 别 | 男 | ||
最高学历 | 研究生 | ||
最高学位 | 博士 | ||
职 务 | |||
职 称 | 教授、博士生导师 | ||
联系方式 | guanqy@lzu.edu.cn | ||
所在部门 | 资源环境学院环境工程研究所 | ||
研究方向 | 大气颗粒物与干旱区环境;第四纪沉积与环境;土壤环境生物地球化学循环过程 | ||
学习经历 | |||
工作经历 | |||
主讲课程 | |||
学术组织兼职 | |||
研究成果 | |||
获得荣誉 |
1. 2005年获兰州大学教学成果一等奖(4/5)
2. 2006年获兰州大学首届 “最受学生爱戴的教师”
3. 2次(2004-2005年、2005-2006年)荣获兰州大学“优秀班主任”
4. 荣获兰州大学2007年度“隆基青年教师教学新秀奖”
5. 2007~2011以及2013年6次年终考核“优秀”。
6. 2008年获甘肃省自然科学二等奖(3/5)
7. 2010年所参与的《地貌学》课程荣获“国家精品课程”(4/10)
8. 荣获西部环境教育部重点实验室2010年度“西部环境奖——青年教师创新奖”
9. 2011年入选教育部“新世纪优秀人才支持计划”
10. 荣获2011年度、2012年度兰州大学创新创业行动计划“优秀指导教师”
11. 荣获兰州大学2011年度“隆基中青年教师教学骨干奖”
12. 2013年被宝钢教育基金会授予“宝钢优秀教师奖”。
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在研项目 | 现主持一项国家自然科学基金、一项教育部新世纪优秀人才基金,一项中央高校基本科研业务费专项资金(重点项目),作为主要成员参与一项“973”课题、一项国家自然科学基金重点项目。主持过一项国家自然科学基金、一项甘肃省自然科学基金、一项中央高校基本科研业务费专项资金,作为主要成员参与过多项国家自然科学基金、省部级基金及“973”课题。 | ||
发表论文 |
发表和合作发表科研论文52篇(SCI收录22篇,EI收录5篇),其中以本人为主发表科研论文23篇,主要论文有:
2. 2. Guan, Q.Y., Wang, L.J., Wang, L., Pan, B.T., Zhao, S.L., Zheng, Y., 2014. Analysis of trace elements (heavy-metal-based) in the surface soils of a desert-loess transitional zone in the south of the Tengger Desert. Environment Earth Sciences, 72(8), 3015-3023.(SCI-4)
3. 3.Pan, B.T., Guan, Q.Y.*( 通讯作者), Gao, H.S., Guan, D.S., Liu, F.L., Li, Z.M., Su, H., 2014. The origin and sources of loess-like sediment in the JinshaRiverValley, southwest China. Boreas, 43, 121-131. (SCI-2)
4. 4.Guan, Q.Y., Zhang, J.D., Wang, L.J., Pan, B.T., Gui, H.J., Zhang, C., 2013. Discussion of the relationship between dustfall grain size and the desert border, taking the southern border of the Tengger Desert and the southern dust deposit area as an example. Palaeogeography, Palaeoclimatology, Palaeoecology, 386, 1-7. (SCI-2)
5. 5.Guan, Q.Y., Wang, L.J., Gui, H.J., Pan, B.T., Zhang, J.D., 2013. The relationship between modern meteorological elements and the southern border of the TenggerDesert. Theoretical and Applied Climatology, 112, 461-467. (SCI-3)
6. 6.Guan, Q.Y., Pan, B.T., Yang, J., Wang, L.J., Zhao, S.L., Gui, H.J., 2013. The processes and mechanisms of severe sandstorm development in the eastern Hexi Corridor China, during the Last Glacial period. Journal of Asian Earth Sciences, 62, 769-775. (SCI-3)
7. 7.Guan, Q.Y., Pan, B.T., Li, N., Zhang, J.D., Xue, L.J., 2011. Timing and significance of the initiation of present day deserts in the northeastern Hexi Corridor, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 306, 70-74. (SCI-2)
8. 8.Guan, Q.Y., Pan, B.T., Li, N., Li, Q., Hu, Z.B., Gao, H.S., Xu, S.J., Wang, Y., 2010. An indicator of sand storms in the south of the Tengger Desert. Theoretical and Applied Climatology, 102, 197-203. (SCI-3)
9. 9.Guan, Q.Y., Pan, B.T., Li, N., Li, Q., Zhang, J.D., Xu, S.J., Gao, H.S., Liu, J., 2010. Loess record of the evolution history of severe sandstorms in the TenggerDesert during the Last Interglacial Period (MIS5). Geosciences Journal, 14(2), 155-162. (SCI-4)
10. 10.Guan, Q.Y., Pan, B.T., Li, N., Li, Q., Zhang, J.D., Gao, H.S., Liu, J., 2010. Pattern of abrupt climatic fluctuation in the East Asian Monsoon during the last glacial: evidence from Chinese loess records. Comptes Rendus Geoscience, 342(3), 189-196. (SCI-3)
11. 11.Guan, Q.Y., Pan, B.T., Li, N., Li, Q., Zhang, J.D., Gao, H.S., Liu, J., 2010. A warming interval during the MIS 5a/4 transition in two high-resolution loess sections from China. Journal of Asian Earth Sciences, 38, 255-261. (SCI-3)
12. 12. Guan, Q.Y., Pan, B.T., Li, N., Gao. H.S., Li, Q., Yang, X.Y., 2009. Differences among sub-orbital time scale events recorded in two high-resolution loess sections, China, during the last deglaciation. Quaternary International, 198, 246-254. (SCI-3)
13. 13.Guan, Q.Y., Pan, B.T., Gao. H.S., Li, N., Zhang, H., Wang, J.P., 2008. Geochemical evidence of the Chinese loess provenance during the Late Pleistocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 270, 53-58. (SCI-2)
14. 14.Guan, Q.Y., Pan, B.T., Gao, H.S., Li, B.Y., Wang, J.P., Su, H., 2007. Instability characteristics of the East Asian Monsoon recorded by high-resolution loess sections from the last interglacial (MIS5). Science in China (Series D), 50 (7), 1067-1075. (SCI-4 & EI).
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