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分類:導師信息 來源:中國考研網 2015-07-25 相關院校:蘭州大學
姓 名
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張家武
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性 別
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男
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最高學歷
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研究生
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最高學位
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博士
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職 務
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無
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職 稱
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教授
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聯系方式
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jwzhang@lzu.edu.cn
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所在部門
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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-湖泊沉積與環境變化
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學習經歷
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1990.09—1994.06:安徽師范大學地理系本科,獲理學學士學位;
1994.09—1997.07:中國科學院寒區旱區環境與工程研究,所自然地理專業、風沙地貌研究方向碩士,獲理學碩士學位
1997.09—2001.06:蘭州大學資源環境學院自然地理專業、環境變化研究方向博士,獲理學博士學位,導師:陳發虎 教授;其間
1999.10—2000.03:受英國British Council資助,英國倫敦大學環境變化研究中心(ECRC,UCL),介形蟲殼體地球化學科研培訓。
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工作經歷
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2001年獲得博士學位后留蘭州大學工作至今,其中
2001.07—2002.12:蘭州大學資源環境學院自然地理研究所,講師,教學與科研;
2003.01—2003.12:受英國皇家學會資助,英國倫敦大學環境變化研究中心(ECRC,UCL)博士后,合作者Jonathan A. Holmes教授;
2004.03—2004.09:國家自然科學基金委員會地球科學部地理學科,兼聘,國家自然科學基金項目管理;
2005.08—2005.12:受國家留學基金委資助(高校骨干教師項目),英國曼徹斯特大學訪問學者,理工科英語教學培訓(TSEE);
2006.01—2011.12:蘭州大學資源環境學院自然地理研究所,副教授,教學與科研;
2011.01—今蘭州大學資源環境學院自然地理研究所,教授,教學與科研。
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主講課程
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專業英語
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學術兼職
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《Frontiers of Earth Science》編委;QSR、QI、JoP、The Holocene、CSB等SCI期刊評審人,國家自然科學基金項目(D104;D209)函評專家。
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研究成果
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介形蟲殼體穩定同位素與微量元素記錄區域氣候變化;季風區湖泊沉積物自生碳酸鹽穩定同位素;湖泊沉積物無機碳14C年代學
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獲得榮譽
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2011年獲教育部“新世紀優秀人才”資助
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在研項目
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主持《青藏高原東北部高山湖泊記錄的全新世氣候與環境變化》(批準號:41271220);
參加科技部973項目《湖泊與濕地生態系統對全球變化的響應及生態恢復對策研究》第二課題《西北干旱區湖泊水文-生態系統演變過程與機制》(課題號:2012CB956102;課題負責人趙艷教授;項目首席:沈吉研究員)
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發表論文
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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.
張家武,王君蘭,郭小燕,李雙,何晶,陳碩,黃小忠,陳發虎,2010. 博斯騰湖全新世巖芯沉積物碳酸鹽氧同位素氣候意義. 第四紀研究,30(6): 1078–1087.
張家武,何晶,陳碩,李雙,2009. 第四紀湖相介形類殼體化石在古環境中的應用——種屬組合研究進展與問題. 地球科學進展,24(11): 1229–1237.
張家武,趙艷,楊太保,陳發虎,2006. 自然地理學專業研究生課程教學管理探析. 高等理科教育, 69(5): 55–58.
張家武,金明,陳發虎,R.W. Battarbee,A.C.G. Henderson,2004. 青海湖沉積巖芯記錄的青藏高原東北部過去800年以來的降水變化. 科學通報,49(1):10–14.
張家武,陳廣庭,陳發虎,王建民,1999,塔克拉瑪干沙漠中部地區線形沙丘表面動力過程,中國沙漠,(1):128-133.
陳發虎,張家武,程波,楊太保,2012. 青海共和盆地達連海晚第四紀高湖面與末次冰消期以來的環境變化. 第四紀研究, 32(1): 122–131.
王君蘭,李暉,鄧偉,郭小燕,李雙,張家武,2012. 內蒙古嘎順諾爾湖泊沉積物磁化率與粒度的古環境意義. 中國沙漠, 32(3): 661–668.
李雙,陳碩,張家武,2010. 紅堿淖湖泊沉積記錄的近五十年來的環境變化. 安徽農業科學, 38(5): 2524–2537.
程波,陳發虎,張家武,2010. 共和盆地末次冰消期以來的植被和環境演變. 地理學報, 65(11):1336–1344.
饒志國,朱照宇,賈國東,陳發虎,Barton Loukas,張家武,強明瑞,2010. 環北太平洋地區現代植物中C3/C4植物相對豐度與氣候條件關系研. 究科學通報, 55(12): 1134–1140.
陳建徽,陳發虎,張恩樓,Stephen Brooks,周愛鋒,張家武, 2009. 柴達木盆地蘇干湖年紋層巖芯搖蚊記錄的過去1000年干旱區濕度變化及其意義. 科學通報, 54(20): 3127–3135.
饒志國,賈國東,朱照宇,吳翼,張家武, 2008. 中國東部表土總有機質碳同位素和長鏈正構烷烴碳同位素的對比研究及其意義. 科學通報, 53(17): 2077–2084.
陳建徽,陳發虎,張家武,楊保,2008. 中國西北干旱區小冰期的濕度變化特征. 地理學報, 63(1): 23–33.
陳發虎,黃小忠,張家武, Holmes J.A.,陳建徽,2007. 新疆博斯騰湖記錄的內陸干旱區小冰期濕潤氣候研究. 中國科學(D輯), 37(1): 77–85.
肖舜,陳發虎,強明瑞,張家武,周愛鋒,孫東懷,2007. 青海蘇干湖表層沉積物粒度分布模式與大氣粉塵記錄. 地理學報, 62(11): 1143–1154.
周愛鋒,陳發虎,強明瑞,楊美臨,張家武,2007. 內陸干旱區柴達木盆地蘇干湖年紋層的發現 及其意義. 中國科學(D輯), 37(7): 1–8.
曹潔,張家武,張成君,陳發虎,2007. 青藏高原北緣哈拉湖近800年湖泊沉積及其環境意義. 第四紀研究, 27(1): 100–107.
陳發虎,饒志國,張家武,金明,馬劍英,2006. 隴西黃土高原末次冰期有機碳同位素變化及其意義. 科學通報, 51(11): 1310–1317.
夏敦勝,魏海濤,馬劍英,王訓明,張家武,趙暉,2006. 中亞地區現代表土磁學特征及其古環境意義. 第四紀研究, 26(6): 937–946.
強明瑞,魯瑞潔,張家武,肖舜,陳發虎,2006. 柴達木盆地蘇干湖表層沉積與塵暴事件——元素示蹤的初步結果. 湖泊科學, 18(6): 590–596.
強明瑞,陳發虎,周愛鋒,肖舜,張家武,金明,2006. 蘇干湖沉積物粒度組成記錄塵暴事件的初步研究. 第四紀研究, 26(6): 915–922.
饒志國,陳發虎,汪海斌,張家武,朱照宇,2006. 九州臺古土壤S1記錄的末次間冰期東亞夏季風變化. 海洋地質與第四紀地質, 26(2): 103–111.
強明瑞,陳發虎,張家武,高尚玉,周愛鋒,2005. 2ka蘇干湖沉積碳酸鹽穩定同位素記錄的氣候變化. 科學通報, 50(3): 1385–1393.
饒志國,朱照宇,陳發虎,張家武,2005. 黃土有機質穩定碳同位素研究進展. 地球科學進展, 20(12): 126–133.
陳發虎,程波,朱艷,陳發虎,張家武,黃小忠,楊美臨,2004. 石羊河流域表土抱粉與植被的關系. 冰川凍土, 26(1): 81–88.
冷疏影,宋長青,張立新,劉黎明,張家武,李仁杰,2004. 2004年度地理學基金項目評審及成果分析,地球科學進展,19(6): 1006–1009.
程波,朱艷,陳發虎,張家武,黃小忠,楊美臨,2004. 石羊河流域表土抱粉與植被的關系,冰川凍土,26(1): 81–88.
朱艷,程波,陳發虎,張家武,2004. 石羊河流寓現代孢粉傳播研究. 科學通報,49(1): 15–21.
陳一萌,饒志國,張家武,陳興盛,周愛鋒,2004. 臨夏塬堡黃土剖面晚馬蘭黃土地層劃分和形成時代,中國沙漠, (5): 539–543.
陳一萌,饒志國,張家武,陳興盛,2004. 中國黃土高原西部馬蘭黃土記錄的MIS3氣候特征與全球氣候記錄的對比研究,第四紀研究,(3): 359–365.
汪海斌,陳發虎,張家武,2002. 黃土高原西部地區黃土粒度的環境指示意義,中國沙漠,22(1): 1–6.
吳海斌,郭正堂,方小敏,張家武,陳發虎,2002. 250 kaBP前后中國北方干旱區的擴張及其原因,科學通報,47(17): 1341–1346.
朱艷,陳發虎,張家武,安成邦,2001. 干旱區沉積環境對孢粉組合影響的初步研究—以石羊河流域為例. 沉積學報, 19(2):186-191.
朱艷,陳發虎,張家武,安成邦,2001. 距今五千年左右環境惡化事件對我國新石器文化的影響及其原因的初步探討。地理科學進展,20(2): 111–121.
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