Oasen Drinking Water Company, PO box 122, 2800 AC Gouda, The Netherlands.
Water Res. 2012 Mar 15;46(4):1061-9. doi: 10.1016/j.watres.2011.11.075. Epub 2011 Dec 8.
Phosphorus limitation has been demonstrated for heterotrophic growth in groundwater, in drinking water production and distribution systems, and for nitrification of surface water treatment at low temperatures. In this study, phosphorus limitation was tested, in the Netherlands, for nitrification of anaerobic groundwater rich in iron, ammonium and orthophosphate. The bioassay method developed by Lehtola et al. (1999) was adapted to determine the microbially available phosphorus (MAP) for nitrification. In standardized batch experiments with an enriched mixed culture inoculum, the formation of nitrite and nitrate and ATP and the growth of ammonia-oxidizing bacteria (AOB; as indicated by qPCR targeting the amoA-coding gene) were determined for MAP concentrations between 0 and 100 μg PO4-P L(-1). The nitrification and microbial growth rates were limited at under 100 μg PO4-P L(-1) and virtually stopped at under 10 μg PO4-P L(-1). In the range between 10 and 50 μg PO4-P L(-1), a linear relationship was found between MAP and the maximum nitrification rate. AOB cell growth and ATP formation were proportional to the total ammonia oxidized. Contrary to Lehtola et al. (1999), biological growth was very slow for MAP concentrations less than 25 μg PO4-P L(-1). No full conversion nor maximum cell numbers were reached within 19 days. In full-scale groundwater filters, most of the orthophosphate was removed alongside with iron. The remaining orthophosphate appeared to have only limited availability for microbial growth and activity. In some groundwater filters, nitrification was almost totally prevented by limitation of MAP. In batch experiments with filtrate water from these filters, the nitrification process could be effectively stimulated by adding phosphoric acid.
磷限制已被证明存在于地下水的异养生长、饮用水生产和分配系统以及低温地表水的硝化作用中。在这项研究中,在荷兰,对富含铁、铵和正磷酸盐的厌氧地下水的硝化作用进行了磷限制测试。Lehtola 等人(1999 年)开发的生物测定方法被改编用于确定硝化作用中微生物可利用的磷(MAP)。在标准化的分批实验中,使用富含有机物的混合培养接种物,确定了在 0 到 100 μg PO4-P L(-1) 之间 MAP 浓度下亚硝酸盐和硝酸盐的形成以及 ATP 的产生和氨氧化细菌(AOB;通过靶向 amoA 编码基因的 qPCR 进行指示)的生长。在低于 100 μg PO4-P L(-1) 的情况下,硝化作用和微生物生长速率受到限制,在低于 10 μg PO4-P L(-1) 的情况下几乎停止。在 10 到 50 μg PO4-P L(-1) 之间,MAP 与最大硝化速率之间存在线性关系。AOB 细胞生长和 ATP 形成与总氨氧化成正比。与 Lehtola 等人(1999 年)不同的是,对于 MAP 浓度小于 25 μg PO4-P L(-1),生物生长非常缓慢。在 19 天内,没有达到完全转化或最大细胞数量。在地下水过滤器中,大部分正磷酸盐与铁一起被去除。剩余的正磷酸盐似乎对微生物生长和活性的可用性有限。在一些地下水过滤器中,由于 MAP 的限制,硝化作用几乎完全被阻止。在这些过滤器的滤液的批量实验中,通过添加磷酸可以有效地刺激硝化作用过程。