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Nitrogen removal in maturation waste stabilisation ponds via biological uptake and sedimentation of dead biomass

机译:通过生物吸收和沉淀死生物质来去除成熟废物稳定池中的氮

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In this work a set of experiments was undertaken in a pilot-scale WSP system to determine the importance of organic nitrogen sedimentation on ammonium and total nitrogen removals in maturation ponds and its seasonal variation under British weather conditions, from September 2004 to May 2007. The nitrogen content in collected sediment samples varied from 4.17% to 6,78% (dry weight) and calculated nitrogen sedimentation rates ranged from 273 to 2868 g N/had. High ammonium removals were observed together with high concentrations of chlorophyll-a in the pond effluent. Moreover, chlorophyll-a had a very good correlation with the corresponding increment of VSS (algal biomass) and suspended organic nitrogen (biological nitrogen uptake) in the maturation pond effluents. Therefore, when ammonium removal reached its maximum, total nitrogen removal was very poor as most of the ammonia taken up by algae was washed out in the pond effluent in the form of suspended solids. After sedimentation of the dead algal biomass, it was clear that algal-cell nitrogen was recycled from the sludge layer into the pond water column. Recycled nitrogen can either be taken up by algae or washed out in the pond effluent. Biological (mainly algal) uptake of inorganic nitrogen species and further sedimentation of dead biomass (together with its subsequent mineralization) is one of the major mechanisms controlling in-pond nitrogen recycling in maturation WSP, particularly when environmental and operational conditions are favourable for algal growth.
机译:在这项工作中,在2004年9月至2007年5月期间,在中试规模的WSP系统中进行了一组实验,以确定有机氮沉降对成熟池中铵和总氮去除的重要性及其在英国天气条件下的季节性变化。收集的沉积物样品中的氮含量为4.17%至6,78%(干重),计算出的氮沉降速率为273至2868 g N / had。池塘污水中氨去除率高,叶绿素-a浓度高。此外,叶绿素a与成熟池流出物中的VSS(藻类生物量)和悬浮的有机氮(生物氮吸收)的相应增量具有很好的相关性。因此,当铵去除达到最大值时,总氮去除非常差,因为藻类吸收的大部分氨都以悬浮固体的形式从池塘流出物中冲出。沉淀的藻类生物质沉淀后,很明显藻类细胞的氮从污泥层再循环到池塘水柱中。再循环的氮既可以被藻类吸收,也可以在池塘污水中被冲洗掉。无机氮物种的生物(主要是藻类)吸收以及死生物质的进一步沉淀(及其随后的矿化)是控制成熟WSP进行适时氮循环的主要机制之一,特别是当环境和操作条件有利于藻类生长时。

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