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中国西南高原湖泊沉积物/水界面附近氮、磷和硅的再生

Regeneration of N, P and Si near the sediment/water interface of lakes from Southwestern China Plateau.

作者信息

Wu F, Qing H, Wan G

机构信息

State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550002, People's Republic of China.

出版信息

Water Res. 2001 Apr;35(5):1334-7. doi: 10.1016/s0043-1354(00)00380-8.

Abstract

Lake water, pore water, and sediments were sampled in both polluted and unpolluted lakes from Southwestern (SW) China Plateau. The results show that although the mechanisms of nutrient regeneration were similar in the polluted and unpolluted lakes, the processes, however, were much stronger in the polluted lakes. Nitrogen regeneration was mainly of organic process. Phosphorus regeneration was essentially controlled by iron redox cycling near sediment/water interface. Nutrient upward fluxes were in the order SiO2 > NH4+ > PO4(3-). This study has significance for further investigating the response of nutrient biogeochemistry to the increasing nutrient levels in aquatic environments.

摘要

在中国西南高原的污染湖泊和未污染湖泊中采集了湖水、孔隙水和沉积物样本。结果表明,尽管污染湖泊和未污染湖泊中营养物质再生的机制相似,但污染湖泊中的这些过程更为强烈。氮再生主要是有机过程。磷再生基本上受沉积物/水界面附近铁的氧化还原循环控制。营养物质向上通量的顺序为SiO2 > NH4+ > PO4(3-)。本研究对于进一步研究水生环境中营养生物地球化学对营养水平增加的响应具有重要意义。

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