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通过生物吸收和死生物质的沉淀从成熟废水稳定池中去除氮。

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

机构信息

Sección de Saneamiento Ambiental, Universidad Nacional de Colombia, Bogotá, Colombia.

出版信息

Water Sci Technol. 2010;61(4):1027-34. doi: 10.2166/wst.2010.952.

DOI:10.2166/wst.2010.952
PMID:20182083
Abstract

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/ha d. 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.

摘要

在本工作中,进行了一组中试规模的 WSP 系统实验,以确定在英国天气条件下,有机氮沉淀对沉淀塘中氨氮和总氮去除的重要性及其季节性变化,实验时间为 2004 年 9 月至 2007 年 5 月。采集的沉积物样品中的氮含量从 4.17%到 6.78%(干重)不等,计算出的氮沉淀速率从 273 到 2868 g N/ha d 不等。在池塘出水中观察到高的氨氮去除率和高浓度的叶绿素-a。此外,叶绿素-a 与成熟池塘出水中相应的 VSS(藻类生物量)和悬浮有机氮(生物氮吸收)的增量具有很好的相关性。因此,当氨氮去除达到最大值时,总氮去除效果很差,因为藻类吸收的大部分氨以悬浮固体的形式从池塘出水中被冲刷出去。在死藻生物量沉淀后,显然藻类细胞氮从污泥层被重新循环到池塘水层中。回收的氮可以被藻类吸收,也可以从池塘出水中被冲刷出去。生物(主要是藻类)对无机氮的吸收和死生物质的进一步沉淀(以及随后的矿化)是控制沉淀塘中氮循环的主要机制之一,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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