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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化池中的氮

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In this work a set of experiments was undertaken in a pilot-scale WSP system to determinenthe importance of organic nitrogen sedimentation on ammonium and total nitrogen removalsnin maturation ponds and its seasonal variation under British weather conditions, from Septembern2004 to May 2007. The nitrogen content in collected sediment samples varied from 4.17% ton6.78% (dry weight) and calculated nitrogen sedimentation rates ranged from 273 to 2868 g N/ha d.nHigh ammonium removals were observed together with high concentrations of chlorophyll-a innthe pond effluent. Moreover, chlorophyll-a had a very good correlation with the correspondingnincrement of VSS (algal biomass) and suspended organic nitrogen (biological nitrogen uptake)nin the maturation pond effluents. Therefore, when ammonium removal reached its maximum,ntotal nitrogen removal was very poor as most of the ammonia taken up by algae was washednout in the pond effluent in the form of suspended solids. After sedimentation of the dead algalnbiomass, it was clear that algal-cell nitrogen was recycled from the sludge layer into the pondnwater column. Recycled nitrogen can either be taken up by algae or washed out in the pondneffluent. Biological (mainly algal) uptake of inorganic nitrogen species and further sedimentationnof dead biomass (together with its subsequent mineralization) is one of the major mechanismsncontrolling in-pond nitrogen recycling in maturation WSP, particularly when environmental andnoperational conditions are favourable for algal growth.
机译:在这项工作中,在中试规模的WSP系统中进行了一组实验,以确定在2004年9月至2007年5月英国成熟天气下,有机氮沉降对铵态氮和总氮去除量的重要性以及成熟期池塘的季节性变化。收集的沉积物样品的变化范围为4.17%ton6.78%(干重),计算出的氮沉降速率范围为273至2868 g N / had。n在池塘污水中观察到高的铵去除率和高浓度的叶绿素a。此外,叶绿素-a与成熟池污水中VSS(藻类生物量)和悬浮有机氮(生物氮吸收)的相应增加非常相关。因此,当铵去除达到最大时,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被冲洗掉在池塘流出物中。死藻生物质沉淀后,很明显藻细胞中的氮从污泥层再循环到池水塔中。再循环的氮可以被藻类吸收,也可以在污水中冲洗掉。无机氮物质的生物(主要是藻类)吸收以及死生物质的进一步沉淀(以及随后的矿化)是控制WSP成熟期中进行中氮循环利用的主要机制之一,特别是在环境和操作条件有利于藻类生长的情况下。

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