男,1973年7月出生,山西中阳人,博士,自然地理研究所教授。研究方向为干旱区环境演变
湖泊沉积与大气粉尘。近年来,主要探讨了
末次冰期以来
腾格里沙漠东南缘风成沉积与沙漠环境演化,末次冰消
期东亚季风
西北缘区气候快速变化事件;利用
苏干湖沉积重建近8 ka来气候变化序列,着重探讨了2 ka来气候变化历史;初步理解了
柴达木盆地封闭湖泊沉积记录
尘暴事件与源区粉尘释放的模式、重建了柴达木盆地全新 世尘暴演化历史。主持国家自然科学基金项目、中国博士后科学基金各1项,经费30余万元,参加国家自然科学基金、“973”等项目5项,发表论文10余篇,获
中国地理学会青年优秀论文奖1项。
学习工作经历
1992.9~1996.7
山西师范大学地理系 本科
1996.9~1999.7
中国科学院兰州沙漠研究所 自然地理学 硕士
1999.9~2002.12
兰州大学 自然地理学 博士
2003.7~2005.9
北京师范大学 地理学 博士后研究
2005.9~2008
兰州大学资源环境学院/西部环境教育部重点实验室 副教授
2008至今 兰州大学资源环境学院/西部环境教育部重点实验室 教授
在研项目
1.“新世纪优秀人才支持计划”,教育部,50万元,负责人;
2.“创新群体”项目第一期、第二期与第三期:青藏高原和中东亚干旱区环境变化与地表过程研究(批准号:40421101,40721061),2005.1-2011.12,国家
中华人民共和国国家自然科学基金委员会,20万元,主要参加者;
3.世界各地黄土
磁化率与古气候不同关系机制以及古气候重建问题系统研究(No. 40830105),2009.1-2012.12,国家自然科学基金重点项目,165万元,主要参加者;
4.国家“973”项目,
黄河上游沙漠宽谷段风沙水沙过程与调控机理(No. 2011CB403300)。第一课题“黄河上游沙漠宽谷段粗沙来源与沉积时空特征(No. 2011CB403301)”,2011.1-2015.12,475万元,主要参加人;
发表论文
1.Mingrui Qiang, Fahu Chen, Zhenting Wang, Guangming Niu, Lei Song, 2010. Aeolian deposits at the southeastern margin of the Tengger Desert (China): Implications for
surface wind
strength in the Asian dust source
面积 over the past 20,000 years. Palaeogeography, Palaeoclimatology, Palaeoecology 286, 66-80.
2. Qiang, M.,Lang, L., Wang, Z., 2010. Do fine-grained components of loess indicate westerlies: Insights from observations of dust storm deposits at Lenghu (Qaidam Basin, China). Journal of Arid Environments 74, 1232-1239.
3. Mingrui Qiang, Fahu Chen, Jiawu Zhang, Ruiping Zu, Ming Jin, Aifeng Zhou, Shun Xiao, 2007. Grain size in sediments from Lake Sugan: a possible linkage to dust storm events at the northern margin of the Qinghai–Tibetan
高原 Environmental Geology 51(7), 1229-1238.
4. Mingrui Qiang, Fahu Chen, Aifeng Zhou, Shun Xiao, Jiawu Zhang, Zhenting Wang, 2007. Impacts of wind velocity on sand and dust deposition during dust storm as inferred from a series of observations in the northeastern Qinghai–Tibetan Plateau, China. Powder Technology 175, 82-89.
5. Qiang Mingrui, Chen Fahu, Zhang Jiawu, Gao Shangyu, Zhou Aifeng, 2005. Climatic changes documented by stable isotopes of sedimentary carbonate in Lake Sugan, northeastern Tibetan Plateau of China, since 2 ka BP. Chinese Science Bulletin, 50(17), 1930-1939.
6. Qiang Ming-rui, Li Sen, Gao Shang-yu, 2004. Evidence for abrupt climatic changes on the northwestern margin of the East Asian monsoon during the last Deglaciation. Chinese Geographical Science 14(2), 117-121.
7.F. H. Chen, M. R. Qiang, Z. D. Feng et al., 2003. Stable East Asian monsoon climate during the last interglacial (Eemian) indicated by paleosol S1 in the western part of the Chinese Loess
高原 Global and Planetary Change 36(3), 171-179.
8.Gao Shangyu, Lu Ruijie, Qiang Mingrui, et al. Reconstruction of precipitation in the last 140 years from tree ring at south margin of the Tengger Desert, China. Chinese Science Bulletin, 2005, 50(21): 2487-2492
9.Zhou AiFeng, Chen FaHu, Qiang MingRui, Yang MeiLin, Zhang JiaWu, 2007. The discovery of annually laminated sediments (varves) from shallow Sugan Lake in inland arid China and their paleoclimatic significance. Science in China (D Series) 50(8), 1218-1224.
10.Ruiping Zu, Xian Xue, Mingrui Qiang, Bao Yang, Jianjun Qu, Kecun Zhang, 2008. Characteristics of near-
surface wind regimes in the Taklimakan Desert, China. Geomorphology 96, 39–47.
参考资料
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