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龙感湖沉积物碳、氮同位素记录的环境演化

周志华1,2;李军1;朱兆洲3   

  1. 1中国科学院地球化学研究所 环境地球化学国家重点实验室, 贵阳 550002;2中国科学院研究生院, 北京 100039;3天津师范大学 水环境与水资源重点实验室, 天津 300074
  • 收稿日期:2006-09-13 修回日期:1900-01-01 出版日期:2007-05-08 发布日期:2007-05-08

Environmental evolution of Longgan Lake sediments recorded by carbon and nitrogen isotopes.

ZHOU Zhi-hua1,2; LI Jun1; ZHU Zhao-zhou3   

  1. 1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China;2Graduate University of Chinese Academy of Sciences, Beijing 100039, China;3Key Laboratory of Aqueous Environment and Water Resource, Tianjin Normal University, Tianjin 300074, China
  • Received:2006-09-13 Revised:1900-01-01 Online:2007-05-08 Published:2007-05-08

摘要: 通过对龙感湖沉积物样品中δ13Corg、δ15N、有机碳与总氮比值(C/N)、总有机碳(TOC)和总氮(TN)含量的测定,分析了自1948年以来龙感湖沉积物有机质的来源,探讨了湖泊生产力变化以及随后的沉积演化过程。结果表明:在这个沉积历史阶段中,湖泊沉积物有机质以自生有机物源为主,大型水草发育,伴有低等藻类参与,湖泊沉积物受陆源输入影响较小,基本不受城市污染物的输入影响,但受流域农业化肥大量使用的影响较大;随着营养物质的输入,湖泊的初级生产力逐渐增大,藻类开始发育;在沉积历史上L2点附近低等藻类相对发育早,但L1点沉积物相对能够固定更多的营养盐。

关键词: 年龄结构, 生命表, 存活曲线, 环境因子, 时间序列

Abstract: Through the determinations of δ13Corg, δ15N, total organic C, total N and C/N ratio in Longgan Lake sediments, this paper analyzed the sources of sedimentary organic matters in the Lake, variations of lake productivity, and evolution process of sediment since 1948. The results showed that the sedimentary organic matters mainly derived from native aquatic organic matters. The aquatic plants were float grasses accompaning with algae. Land matters and city pollutants had little influence, while large amounts of applied chemical fertilizers had great effects on the lake sediments. With the input of nutrients, the primary productivity of the lake increased, and algae began to flourish. In the sedimentary history, algae started to grow earlier in site L2 than in site L1, but the sediment in site L1 could fix more nutrients.

Key words: Age structure, Life table, Survival curve, Environmental factor, Time sequence