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Seasonal variation of organic compounds in a eutrophic oxbow lake

机译:富营养牛弓湖中有机化合物的季节性变化

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摘要

In many lakes, high planktonic biomass generates such large quantities that bottom waters become anoxic (Baranovic et al. 1993, Bardosi et al. 2000, Devai et al. 2002, PadisAk et al. 2003), and massive organic-mineral aggregates occur in the water column, depending on meteorological and biochemical conditions in the water column (Stachowitsch et al. 1990; Degobbis et al. 1995). Chemical and physical speciation of dissolved organic carbon (DOC) impact the formation of aggregates in marine environment, but few studies have addressed the speciation of DOC in lacustrine ecosystems (V-Balogh et al. 2003). This study reports seasonal variability of DOC, total dissolved carbohydrates (TDCHO), total dissolved free amino acids (TDFAA), and colloidal organic carbon (COC > 1 kDa) in a eutrophic oxbow lake.
机译:在许多湖泊中,大量的浮游生物量产生大量水,以至于底水变成缺氧的气体(Baranovic等,1993; Bardosi等,2000; Devai等,2002; PadisAk等,2003),大量的有机矿物质聚集在海底。取决于水柱中的气象和生化条件(Stachowitsch等,1990; Degobbis等,1995)。溶解有机碳(DOC)的化学和物理形态影响海洋环境中聚集体的形成,但很少有研究针对湖泊生态系统中DOC的形态(V-Balogh等人2003)。这项研究报告了富营养牛弓湖中DOC,总溶解碳水化合物(TDCHO),总溶解游离氨基酸(TDFAA)和胶体有机碳(COC> 1 kDa)的季节性变化。

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