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CHEN Ping, HE Bao-yin, DU Yun, Kunihiko ENDO, YANG Han-dong. The EnvironmentalMagnetic Records of Honghu Lake Evolution in Past 1200 Years[J]. Acta Sedimentologica Sinica, 2005, 23(1): 138-142.
Citation: CHEN Ping, HE Bao-yin, DU Yun, Kunihiko ENDO, YANG Han-dong. The EnvironmentalMagnetic Records of Honghu Lake Evolution in Past 1200 Years[J]. Acta Sedimentologica Sinica, 2005, 23(1): 138-142.

The EnvironmentalMagnetic Records of Honghu Lake Evolution in Past 1200 Years

  • Received Date: 2004-04-19
  • Rev Recd Date: 2004-09-03
  • Publish Date: 2005-03-10
  • Based on the environmental magnetic measurement on the core with the length of 140cm collected from Honghu Lake, it has been analyzed the chart that the environmental magnetic parameters vary alone with the depth.The result suggests that the stable single domain and fine viscous ferromagnetic minerals dominate the characteristics of sediments. The magnetic minerals grain size increasingly reduces from the bottom to top. By combination AMS dating and geochemistry analyses, it can be deduced that Honghu Lake experiences swampy and lacustrine sediment from last 1200a. Moreovermagnetic characteristics changing corresponds to palaeoclimatic changes. In cold and dry condition,the magnetic parameters are higher than that in warm and wet condition. They record the course that Honghu Lake extends and shrinks along with climate; at one time reflects the human activities' impact on the lake.
  • [1] 1 张卫国,俞立中. 长江口潮摊沉积物的磁学性质及其与粒度的关系[J].中国科学d辑,2002,(09):783-792.

    2 MaherA. Magnetic properties of some synthetic sub-micron magnetites[J].Geophysical Journal of the Royal Astronomical Society,1988.83-96.

    3 孙知明,胡守云,马醒华. 现代沉积物中磁性矿物的研究及其环境意义[J].地球物理学报,1996,(02):178-187.

    4 BoyleJF,Rose N L,Bennion H. Environmental impacts in the Jianghan Plane:evidence from lake sediments[J].Water Air and Soil Pollution,1999.21-40.

    5 蔡述明,石泉. 古云梦泽研究[M].武汉:湖北教育出版社,1996.

    6 中国科学院水生所洪湖课题研究组. 洪湖水体生物生产力综合开发及湖泊生态环境优化研究[M].北京:海洋出版社,1991.123-132.

    7 卢升高,俞劲炎,章明奎. 长江中下游第四纪沉积物发育土壤磁性增强的环境磁学机制[J].沉积学报,2000,(03):336-340.

    8 易朝路,吴显新,刘会平. 长江中湖泊沉积微结构特征与沉积环境[J].沉积学报,2002,(02):293-300.
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  • Received:  2004-04-19
  • Revised:  2004-09-03
  • Published:  2005-03-10

The EnvironmentalMagnetic Records of Honghu Lake Evolution in Past 1200 Years

Abstract: Based on the environmental magnetic measurement on the core with the length of 140cm collected from Honghu Lake, it has been analyzed the chart that the environmental magnetic parameters vary alone with the depth.The result suggests that the stable single domain and fine viscous ferromagnetic minerals dominate the characteristics of sediments. The magnetic minerals grain size increasingly reduces from the bottom to top. By combination AMS dating and geochemistry analyses, it can be deduced that Honghu Lake experiences swampy and lacustrine sediment from last 1200a. Moreovermagnetic characteristics changing corresponds to palaeoclimatic changes. In cold and dry condition,the magnetic parameters are higher than that in warm and wet condition. They record the course that Honghu Lake extends and shrinks along with climate; at one time reflects the human activities' impact on the lake.

CHEN Ping, HE Bao-yin, DU Yun, Kunihiko ENDO, YANG Han-dong. The EnvironmentalMagnetic Records of Honghu Lake Evolution in Past 1200 Years[J]. Acta Sedimentologica Sinica, 2005, 23(1): 138-142.
Citation: CHEN Ping, HE Bao-yin, DU Yun, Kunihiko ENDO, YANG Han-dong. The EnvironmentalMagnetic Records of Honghu Lake Evolution in Past 1200 Years[J]. Acta Sedimentologica Sinica, 2005, 23(1): 138-142.
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