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分类:导师信息 来源:中国半岛真人体育 2015-07-25 相关院校:兰州大学
姓 名
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张家武
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性 别
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男
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最高学历
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研究生
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最高学位
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博士
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职 务
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无
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职 称
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教授
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联系方式
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jwzhang@lzu.edu.cn
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所在部门
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自然地理研究所
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研究方向
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自然地理-湖泊沉积与环境变化
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学习经历
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1990.09—1994.06:安徽师范大学地理系本科,获理学学士学位;
1994.09—1997.07:中国科学院寒区旱区环境与工程研究,所自然地理专业、风沙地貌研究方向硕士,获理学硕士学位
1997.09—2001.06:兰州大学资源环境学院自然地理专业、环境变化研究方向博士,获理学博士学位,导师:陈发虎 教授;其间
1999.10—2000.03:受英国British Council资助,英国伦敦大学环境变化研究中心(ECRC,UCL),介形虫壳体地球化学科研培训。
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工作经历
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2001年获得博士学位后留兰州大学工作至今,其中
2001.07—2002.12:兰州大学资源环境学院自然地理研究所,讲师,教学与科研;
2003.01—2003.12:受英国皇家学会资助,英国伦敦大学环境变化研究中心(ECRC,UCL)博士后,合作者Jonathan A. Holmes教授;
2004.03—2004.09:国家自然科学基金委员会地球科学部地理学科,兼聘,国家自然科学基金项目管理;
2005.08—2005.12:受国家留学基金委资助(高校骨干教师项目),英国曼彻斯特大学访问学者,理工科英语教学培训(TSEE);
2006.01—2011.12:兰州大学资源环境学院自然地理研究所,副教授,教学与科研;
2011.01—今兰州大学资源环境学院自然地理研究所,教授,教学与科研。
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主讲课程
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专业英语
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学术兼职
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《Frontiers of Earth Science》编委;QSR、QI、JoP、The Holocene、CSB等SCI期刊评审人,国家自然科学基金项目(D104;D209)函评专家。
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研究成果
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介形虫壳体稳定同位素与微量元素记录区域气候变化;季风区湖泊沉积物自生碳酸盐稳定同位素;湖泊沉积物无机碳14C年代学
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获得荣誉
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2011年获教育部“新世纪优秀人才”资助
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在研项目
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主持《青藏高原东北部高山湖泊记录的全新世气候与环境变化》(批准号:41271220);
参加科技部973项目《湖泊与湿地生态系统对全球变化的响应及生态恢复对策研究》第二课题《西北干旱区湖泊水文-生态系统演变过程与机制》(课题号:2012CB956102;课题负责人赵艳教授;项目首席:沈吉研究员)
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发表论文
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Zhang J., Chen F., Holmes J.A., Wang J., Li H., Guo X., Li S., Lu Y., Zhao Y., Qiang M., 2011. Holocene monsoon climate documented by oxygen and carbon isotopes from lake sediments and peat bogs in China: a review and synthesis. Quaternary Science Reviews 30, 1973–1987.
Zhang J., Holmes J.A., Chen F., Qiang M., Zhou A., Chen S., 2009. An 850-year ostracod-shell trace-element record from Sugan Lake, northern Tibetan Plateau, China: Implications for interpreting the shell chemistry in high-Mg/Ca waters. Quaternary International 194:119–133.
Zhang J., Chen F., Battarbee R. et al, 2003. High-resolution precipitation variations in the North Tibet Plateau over the last 800 years documented by sediment cores of Lake Qinghai. Chinese Science Bulletin 48(14): 1451–1456.
Cheng B., Chen F., Zhang J., 2013. Palaeovegetational and palaeoenvironmental changes since the last deglacial in Gonghe Basin, northeastern Tibetan Plateau. Journal of Geographical Science, 23(1): 136–146.
Dong G., Zhang F., Ma M., Fan Y., Zhang J., Wang Z., Chen F., 2013. Ancient landslide-dam events in the Jishi Gorge, upper Yellow River valley, China. Quaternary Research, http://dx.doi.org /10.1016/ j.yqres. 2013.09.003.
Wünnemann B., Wagner J., Zhang Y., Yan D, Wang R., Shen Y., Fang X., Zhang J., 2012. Implications of diverse sedimentation patterns in Hala Lake, Qinghai Province, China for reconstructing Late Quaternary climate. Journal of Paleolimnology, 48(4):725–749.
Lü Y., An C., Zhang J., Wang Z., Tao S., Zhao J., 2012. A Holocene dust record in arid central Asia inferred from Lake Barkol, northwest China. Environmental earth sciences, 65(1):213–220.
Wang X., Zhang C., Zhang J., Hua T., Lang L., Zhang X., Wang L., 2010. Nebkha formation: Implications for reconstructing environmental changes over the past several centuries in the Ala Shan Plateau, China. Palaeogeography, Palaeoclimatology, Palaeoecology 297: 697–706.
Wang X., Chen F., Zhang J., Yang Y., Li J., Hasi E., Zhang C., Xia D., 2010. Climate, Desertification, and the Rise and Collapse of China’s Historical Dynasties. Human Ecology, 38(1):157–172.
Rao Z., Zhu Z., Jia G., Chen F., Barton L., Zhang J., Qiang M., 2010. Relationship between climatic conditions and the relative abundance of modern C 3 and C 4 plants in three regions around the North Pacific. Chinese Science Bulletin, 55(18):1931–1936.
Chen J., Chen F., Zhang E., Brooks S., Zhou A., Zhang J., 2009. A 1000–year chironomid–based salinity reconstruction from varved sediments of Sugan Lake, Qaidam Basin, arid Northwest China, and its palaeoclimatic significance. Chinese Science Bulletin, 54(20):3749–3759.
Zhao Y., Yu Z., Chen F., Zhang J., Yang B., 2009. Vegetation response to Holocene climate change in monsoon–influenced region of China. Earth–Science Reviews 97: 242–256.
Wang Z., Zhang J., Zhang Q., Qiang M., Chen F., Ling Y., 2008. Barchans of Minqin: Sediment Transport. Geomorphology 96: 233–238.
Rao Z., Jia G., Zhu Z., Wu Y., Zhang J., 2008. Comparison of the carbon isotope composition of total organic carbon and long-chain n-alkanes from surface soils in eastern China and their significance. Chinese Science Bulletin, 53(24):3921–3927.
Holmes J.A., Zhang J., Chen F., Qiang M., 2007. Paleoclimatic implications of an 850-year oxygen-isotope record from the northern Tibetan Plateau. GEOPHYSICAL RESEARCH LETTERS, VOL.34, L23403, doi:10.1029/2007GL032228,2007
Qiang M., Chen F., Zhang J., Zu R., Jin M., Zhou A., Xiao S., 2007. Grain size in sediments from Lake Sugan: a possible linkage to dust storm events at the northern margin of the Qinghai–Tibetan Plateau. Environmental Geology 51: 1229–1238.
Rao Z., Zhu Z., Zhang J., 2007. Different climatic controls of soil δ13Corg in three mid–lattitude regions of the Northern Hemisphere since the Last Glacial period. Chinese Science Bulletin 52(2):259–266.
Zhou A., Chen F., Qiang M., Yang M., Zhang J., 2007. The discovery of annually laminated sediments (varves) from shallow Sugan Lake in inland arid China and their paleoclimatic significance. Science in China Series D: Earth Sciences 50(8): 1218–1224.
Qiang M., Chen F., Zhou A., Xiao S., Zhang J., Wang Z., 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.
Rao Z., Zhu Z., Chen F., Zhang J., 2006. Does δ13Ccarb of the Chinese loess indicate past C3/C4 abundance? A review of research on stable carbon isotopes of the Chinese loess. Quaternary Science Reviews 25: 2252–2257.
Chen F., Huang X., Zhang J., Holmes J. A., Chen J., 2006. Humid Little Ice Age in arid central Asia documented by Bosten Lake, Xinjiang, China. Chinese Science Bulletin, 49(12): 1280–1290.
Chen F., Rao Z., Zhang J., Jin M., Ma J., 2006. Variations of organic carbon isotopic composition and its environmental significance during the last glacial on western Chinese Loess Plateau. Chinese Science Bulletin 51(3): 1593–1602.
Qiang M., Chen F., Zhang J., Gao S., Zhou A., 2005. Climatic changes documented by stable isotopes of sedimentary carbonate in Lake Sugan, northern Tibetan Plateau of China, since 2 ka BP. Chinese Science Bulletin 50(17): 1930–1939.
Feng Z., Wang H., Olson C., Pope G.A., Chen F., Zhang J., An C., 2004. Chronological discord between the last interglacial paleosol (S1) and its parent material in the Chinese Loess Plateau. Quaternary International 117: 17–26.
Wang X., Dong Z., Yan P., Zhang J., Qian G., 2005. Wind energy environments and dunefield activity in the Chinese deserts. Geomorphology 65: 33–48.
Wang X., Dong Z., Zhang J., Liu L., 2004. Modern dust storms in China: An overview. Journal of Arid Environments 58(4): 559–574.
Wang X., Dong Z., Zhang J., Qu J., 2004. Formation of the complex linear dunes in the central Taklimakan Sand Sea, China. Earth Surface Processes and Landforms, 29(6):677–686.
Mischke S., Herzschuh U., Kürschner H., Fuchs D., Zhang J., Meng F., Sun Z., 2003. Sub–Recent Ostracoda from Qilian Mountains (NW China) and their ecological significance. Limnologica 33: 280–292.
Henderson A.C.G., Holmes J.A., Zhang J., Leng M.J., Carvalho L.R., 2003. A carbon– and oxygen–isotope record of recent environmental change from Qinghai Hu, NE Tibetan Plateau. Chinese Science Bulltein 48(14):1463–1468.
Ma J., Li D., Zhang J., Edmunds W.M., Prudhomme C., 2003. Groundwater recharge and climatic change during the last 1000 years from unsaturated zone of SE Badain Jaran Desert. Chinese Science Bulletin 48(14): 1469–1474.
Wang X., Dong Z., Qu J., Zhang J., Zhao A., 2003. Dynamics processes of a simple linear dune in Taklimakan Sand Sea. Geomorphology 52, 233–241.
Wang X., Dong Z., Zhang J., Qu J., Zhao A., 2003. Grain size characteristics of dune sands in the central Taklimakan Sand Sea. Sedimentary Geology 161: 1–14.
Zhu Y., Xie Y., Cheng B., Chen F., Zhang J., 2003. Pollen transport in the Shiyang River drainage, arid China. Chinese Science Bulletin, 48(14):1499–1506.
Yang B., Braeuning A., Shi Y., Zhang J., 2003. Temperature variations on the Tibetan Plateau over the last two millennia. Chinese Science Bulletin, 48(14):1446–1450.
Wang X., Dong Z., Zhang J., Chen G., 2002. Geomorphology of sand dunes in the northeast Taklimakan Sand Sea. Geomorphology 42: 183–195.
Wang X., Dong Z., Zhang J., Zhao A., 2002. Relations between morphology, airflow, sand flux and particle size on transverse dunes, Taklimakan Sand Sea. Earth Surface Processes and Landforms 27: 515–526.
Wu H., Guo Z., Fang X., Zhang J., Chen F., 2002. Extension of drylands in northern China around 250 kaBP linked with the uplift of the southeast margin of Tibetan Plateau. Chinese Science Bulletin, 47(20):1739–1745.
Zhu Y., Chen F., Cheng B., Zhang J., Madsen D.B., 2002. Pollen Assemblage Features of Modern Water Samples from the Shiyang River Drainage, Arid China. Acta Botanica Sinica 44(3): 367–373.
Chen F., Feng Z., Zhang J., 2000. Loess particle size data indicative of stable winter monsoons during the last interglacial in the Western Part of the Chinese Loess Plateau. Catena 39: 233–244.
Chen F., Feng Z., Zhang J., 2000. Stable winter monsoon during the last interglacial documented by eolian deposits in the western part of the Chinese Loess Plateau. Catena, 39(4): 112–121.
张家武,王君兰,郭小燕,李双,何晶,陈硕,黄小忠,陈发虎,2010. 博斯腾湖全新世岩芯沉积物碳酸盐氧同位素气候意义. 第四纪研究,30(6): 1078–1087.
张家武,何晶,陈硕,李双,2009. 第四纪湖相介形类壳体化石在古环境中的应用——种属组合研究进展与问题. 地球科学进展,24(11): 1229–1237.
张家武,赵艳,杨太保,陈发虎,2006. 自然地理学专业研究生课程教学管理探析. 高等理科教育, 69(5): 55–58.
张家武,金明,陈发虎,R.W. Battarbee,A.C.G. Henderson,2004. 青海湖沉积岩芯记录的青藏高原东北部过去800年以来的降水变化. 科学通报,49(1):10–14.
张家武,陈广庭,陈发虎,王建民,1999,塔克拉玛干沙漠中部地区线形沙丘表面动力过程,中国沙漠,(1):128-133.
陈发虎,张家武,程波,杨太保,2012. 青海共和盆地达连海晚第四纪高湖面与末次冰消期以来的环境变化. 第四纪研究, 32(1): 122–131.
王君兰,李晖,邓伟,郭小燕,李双,张家武,2012. 内蒙古嘎顺诺尔湖泊沉积物磁化率与粒度的古环境意义. 中国沙漠, 32(3): 661–668.
李双,陈硕,张家武,2010. 红碱淖湖泊沉积记录的近五十年来的环境变化. 安徽农业科学, 38(5): 2524–2537.
程波,陈发虎,张家武,2010. 共和盆地末次冰消期以来的植被和环境演变. 地理学报, 65(11):1336–1344.
饶志国,朱照宇,贾国东,陈发虎,Barton Loukas,张家武,强明瑞,2010. 环北太平洋地区现代植物中C3/C4植物相对丰度与气候条件关系研. 究科学通报, 55(12): 1134–1140.
陈建徽,陈发虎,张恩楼,Stephen Brooks,周爱锋,张家武, 2009. 柴达木盆地苏干湖年纹层岩芯摇蚊记录的过去1000年干旱区湿度变化及其意义. 科学通报, 54(20): 3127–3135.
饶志国,贾国东,朱照宇,吴翼,张家武, 2008. 中国东部表土总有机质碳同位素和长链正构烷烃碳同位素的对比研究及其意义. 科学通报, 53(17): 2077–2084.
陈建徽,陈发虎,张家武,杨保,2008. 中国西北干旱区小冰期的湿度变化特征. 地理学报, 63(1): 23–33.
陈发虎,黄小忠,张家武, Holmes J.A.,陈建徽,2007. 新疆博斯腾湖记录的内陆干旱区小冰期湿润气候研究. 中国科学(D辑), 37(1): 77–85.
肖舜,陈发虎,强明瑞,张家武,周爱锋,孙东怀,2007. 青海苏干湖表层沉积物粒度分布模式与大气粉尘记录. 地理学报, 62(11): 1143–1154.
周爱锋,陈发虎,强明瑞,杨美临,张家武,2007. 内陆干旱区柴达木盆地苏干湖年纹层的发现 及其意义. 中国科学(D辑), 37(7): 1–8.
曹洁,张家武,张成君,陈发虎,2007. 青藏高原北缘哈拉湖近800年湖泊沉积及其环境意义. 第四纪研究, 27(1): 100–107.
陈发虎,饶志国,张家武,金明,马剑英,2006. 陇西黄土高原末次冰期有机碳同位素变化及其意义. 科学通报, 51(11): 1310–1317.
夏敦胜,魏海涛,马剑英,王训明,张家武,赵晖,2006. 中亚地区现代表土磁学特征及其古环境意义. 第四纪研究, 26(6): 937–946.
强明瑞,鲁瑞洁,张家武,肖舜,陈发虎,2006. 柴达木盆地苏干湖表层沉积与尘暴事件——元素示踪的初步结果. 湖泊科学, 18(6): 590–596.
强明瑞,陈发虎,周爱锋,肖舜,张家武,金明,2006. 苏干湖沉积物粒度组成记录尘暴事件的初步研究. 第四纪研究, 26(6): 915–922.
饶志国,陈发虎,汪海斌,张家武,朱照宇,2006. 九州台古土壤S1记录的末次间冰期东亚夏季风变化. 海洋地质与第四纪地质, 26(2): 103–111.
强明瑞,陈发虎,张家武,高尚玉,周爱锋,2005. 2ka苏干湖沉积碳酸盐稳定同位素记录的气候变化. 科学通报, 50(3): 1385–1393.
饶志国,朱照宇,陈发虎,张家武,2005. 黄土有机质稳定碳同位素研究进展. 地球科学进展, 20(12): 126–133.
陈发虎,程波,朱艳,陈发虎,张家武,黄小忠,杨美临,2004. 石羊河流域表土抱粉与植被的关系. 冰川冻土, 26(1): 81–88.
冷疏影,宋长青,张立新,刘黎明,张家武,李仁杰,2004. 2004年度地理学基金项目评审及成果分析,地球科学进展,19(6): 1006–1009.
程波,朱艳,陈发虎,张家武,黄小忠,杨美临,2004. 石羊河流域表土抱粉与植被的关系,冰川冻土,26(1): 81–88.
朱艳,程波,陈发虎,张家武,2004. 石羊河流寓现代孢粉传播研究. 科学通报,49(1): 15–21.
陈一萌,饶志国,张家武,陈兴盛,周爱锋,2004. 临夏塬堡黄土剖面晚马兰黄土地层划分和形成时代,中国沙漠, (5): 539–543.
陈一萌,饶志国,张家武,陈兴盛,2004. 中国黄土高原西部马兰黄土记录的MIS3气候特征与全球气候记录的对比研究,第四纪研究,(3): 359–365.
汪海斌,陈发虎,张家武,2002. 黄土高原西部地区黄土粒度的环境指示意义,中国沙漠,22(1): 1–6.
吴海斌,郭正堂,方小敏,张家武,陈发虎,2002. 250 kaBP前后中国北方干旱区的扩张及其原因,科学通报,47(17): 1341–1346.
朱艳,陈发虎,张家武,安成邦,2001. 干旱区沉积环境对孢粉组合影响的初步研究—以石羊河流域为例. 沉积学报, 19(2):186-191.
朱艳,陈发虎,张家武,安成邦,2001. 距今五千年左右环境恶化事件对我国新石器文化的影响及其原因的初步探讨。地理科学进展,20(2): 111–121.
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