School of Ecosystem & Forest Sciences, The University of Melbourne , Burnley, Victoria, Australia 3121.
Environ Sci Technol. 2017 Apr 4;51(7):3703-3713. doi: 10.1021/acs.est.6b05653. Epub 2017 Mar 24.
Stormwater biofilters are dynamic environments, supporting diverse processes that act to capture and transform incoming pollutants. However, beneficial water treatment processes can be accompanied by undesirable greenhouse gas production. This study investigated the potential for nitrous oxide (NO) and methane (CH) generation in dissolved form at the base of laboratory-scale stormwater biofilter columns. The influence of plant presence, species, inflow frequency, and inclusion of a saturated zone and carbon source were studied. Free-draining biofilters remained aerobic with negligible greenhouse gas production during storm events. Designs with a saturated zone were oxygenated at their base by incoming stormwater before anaerobic conditions rapidly re-established, although extended dry periods allowed the reintroduction of oxygen by evapotranspiration. Production of CH and NO in the saturated zone varied significantly in response to plant presence, species, and wetting and drying. Concentrations of NO typically peaked rapidly following stormwater inundation, associated with limited plant root systems and poorer nitrogen removal from biofilter effluent. Production of CH also commenced quickly but continued throughout the anaerobic interevent period and lacked clear relationships with plant characteristics or nitrogen removal performance. Dissolved greenhouse gas concentrations were highly variable, but peak concentrations of NO accounted for <1.5% of the incoming total nitrogen load. While further work is required to measure surface emissions, the potential for substantial release of NO or CH in biofilter effluent appears relatively low.
雨水生物滤池是动态环境,支持多种过程,这些过程可以捕获和转化进入的污染物。然而,有益的水处理过程可能伴随着不良的温室气体产生。本研究调查了在实验室规模雨水生物滤池柱底部以溶解形式产生氧化亚氮(NO)和甲烷(CH)的潜力。研究了植物存在、物种、流入频率以及饱和区和碳源的包含情况的影响。在暴雨事件中,自由排水生物滤池保持好氧状态,温室气体产生可忽略不计。带有饱和区的设计在其底部通过进入的雨水充氧,然后迅速重新建立厌氧条件,尽管延长的干燥期允许通过蒸散重新引入氧气。CH 和 NO 在饱和区的产生对植物存在、物种以及湿-干循环有显著影响。NO 的浓度通常在暴雨淹没后迅速达到峰值,这与有限的植物根系和生物滤池出水的脱氮效果较差有关。CH 的产生也很快开始,但在整个厌氧间歇期持续进行,与植物特征或脱氮性能没有明显关系。溶解的温室气体浓度变化很大,但 NO 的峰值浓度仅占进入总氮负荷的<1.5%。虽然需要进一步的工作来测量表面排放,但生物滤池出水中 NO 或 CH 大量释放的潜力似乎相对较低。