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J4 ›› 2010, Vol. 16 ›› Issue (4): 518-527.

• 地层学与沉积学 • 上一篇    下一篇

桂林岩溶湿地沉积物地球化学元素变化的环境影响因子分析

沈德福 ,李世杰 ,蔡德所,张宏亮 ,赵湘桂,李春海   

  1. 1. 湖泊与环境国家重点实验室,中国科学院 南京地理与湖泊研究所,南京 210008;2. 中国科学院 研究生院,北京 100049;3. 南宁师范大学,南宁 530023
  • 收稿日期:2010-05-19 修回日期:2010-07-23 出版日期:2010-12-20 发布日期:2010-12-20
  • 通讯作者: 李世杰,研究员,博士生导师;
  • 作者简介:沈德福,男,1970年生,博士研究生,从事湖泊资源与环境变化研究;E-mail:robortsdf@163.com
  • 基金资助:

    广西水利“十一五”重点科技项目“漓江水生态系统保护与修复的关键技术研究”子课题“漓江流域天然湿地环境变化过程及
    其保护对策研究”;国家科技部重大基础前期研究专项(2004CCA02900)成果

Element Geochemistry of Lake Sediments from Sihu Lake in Guilin Karst  Wetland Region and Its Environmental Effect

SHEN De-fu, LI Shi-jie, CAI De-suo, ZHANG Hong-liang,ZHAO Xiang-gui   

  1. 1. Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; 2. Graduate School of the Chinese Academy of Sciences, Beijing 100049, China ;3. Nanning Normal University, Nanning 530023, China
  • Received:2010-05-19 Revised:2010-07-23 Online:2010-12-20 Published:2010-12-20

摘要:

       湖泊湿地的环境演变受到多种因素作用的影响。本研究采集桂林岩溶湿地寺湖沉积物,分析了该地区近450年来导致环境变化的影响因子。对岩芯的地球化学元素进行了主成分分析,得出沉积物的化学组成主要受控于流域过程的侵蚀程度、径流与成岩作用强弱、区域背景和人类活动等4个影响因子。其中区域背景和人类活动影响因子所占比重较小,但近年来人类活动影响因子数值迅速增大,表现为磷元素沉积通量迅速增大。地球化学元素含量的变化具有明显的阶段性特征,表明不同的阶段影响因子的作用也不一样。

关键词: 湖泊沉积岩芯, 元素地球化学特征, 环境变化记录, 桂林岩溶湿地

Abstract:

         Sedimentation rates and element concentrations  of core sediments from Sihu Lake are investigated and characteristics
of element geochemistry and environmental change around  this  lake are discussed. By using principal component analysis,  the
geochemical composition factors affecting the sediments of the cores are mainly four: the erosion factor, the watershed runoff and
diagenesis factor, the regional background effect factor and the human activity effect factor. The latter two factors usually account
for smaller proportions. However,  in recent years  the human  factor has rapidly numerical  increase because of quick  increase of
phosphorus contents  in  lake sediments. On  the other hand, variations  in chemical elements obviously have periodic  feature:  the fourth period (0-4 cm, corresponding to 1987-2007), is mainly affected by human activities closely related with regional economic
development. The other earlier  three periods  (4-20 cm, corresponding  to 1894-1987; 20-53 cm, corresponding  to 1703-1894;
53-77 cm, corresponding to 1562-1703) were mainly controlled by climate change.

Key words: lake sedimentary core, element geochemistry, environmental change records, Guilin wetlands

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