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Seasonal variation of potential denitrification rates of surface sediment from Meiliang Bay, Taihu Lake, China

机译:太湖梅梁湾表层沉积物潜在反硝化速率的季节变化。

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The regulatory effects of environmental factors on denitrification were studied in the sediments of Meiliang Bay, Taihu Lake, in a monthly sampling campaign over a one-year period. Denitrification rates were measured in slurries of field samples and enrichment experiments using the acetylene inhibition technique. Sediment denitrification rates in inner bay and outer bay ranged from 2.8 to 51.5 nmol N_2/(g dw (dry weight)·hr) and from 1.5 to 81.1 nmol N_2/(g dw·hr), respectively. Sediment denitrification rates were greatest in the spring and lowest in the summer and early autumn, due primarily to seasonal differences in nitrate concentration and water temperature. For each site, positive and linear relationships were regularly observed between denitrification rate and water column nitrate concentration. Of various environmental factors on denitrification that we assessed, nitrate was determined to be the key factor limiting denitrification rates in the sediments of Meiliang Bay. In addition, at the two sites denitrification rates were also regulated by temperature. The addition of organic substrates had no significant effect on denitrification rate, indicating that sediment denitrification was not limited by organic carbon availability in the sediments. Nitrate in the water column was depleted during summer and early autumn, and this suppressed effective removal of nitrogen from Taihu Lake by denitrification.
机译:在为期一年的每月采样活动中,研究了太湖梅梁湾沉积物中环境因素对反硝化的调节作用。使用乙炔抑制技术在田间样品的浆液和富集实验中测量反硝化率。内湾和外湾的沉积物反硝化率分别为2.8至51.5 nmol N_2 /(g dw(干重)·hr)和1.5至81.1 nmol N_2 /(g dw·hr)。春季的沉积物反硝化率最高,夏季和秋季的初夏沉积物的反硝化率最低,这主要是由于硝酸盐浓度和水温的季节性差异所致。对于每个位置,定期观察到反硝化速率与水柱硝酸盐浓度之间存在正相关和线性关系。在我们评估的各种反硝化环境因素中,硝酸盐被确定为限制美良湾沉积物中反硝化率的关键因素。另外,在两个位置,反硝化速率也受温度调节。有机底物的添加对反硝化率没有显着影响,表明沉积物的反硝化作用不受沉积物中有机碳有效性的限制。在夏季和秋季初,水柱中的硝酸盐被消耗掉了,这抑制了通过反硝化作用从太湖中有效去除氮。

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