Internal Water Storage as a Means of Improving Nitrogen Retention and Reducing Greenhouse Gas Emission in Stormwater Treatment

IF 4.3 Q1 ENVIRONMENTAL SCIENCES ACS ES&T water Pub Date : 2025-02-27 DOI:10.1021/acsestwater.4c00864
Tahiya Tarannum, Bishwodeep Adhikari and Lauren E. McPhillips*, 
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Abstract

Internal water storage (IWS) is gaining interest as a design element in stormwater control measures. It is implemented via an upturned elbow or elevated underdrain to create a subsurface storage zone with saturated conditions conducive to nitrogen removal via denitrification. However, IWS can potentially alter emissions of microbially produced greenhouse gases due to changes in subsurface redox conditions. These greenhouse gases include carbon dioxide, methane, and nitrous oxide. We investigated these biogeochemical dynamics using mesocosms mimicking free draining, IWS, and fully saturated stormwater treatment basins. In a series of simulated storm events, we quantified nitrogen removal, dissolved gas concentrations in the outflow, and surface soil emissions of greenhouse gases. IWS and fully saturated mesocosms had the best nitrate reduction, although fully saturated mesocosms exported other forms of nitrogen. Regarding greenhouse gas emissions, fully saturated mesocosms had the highest methane concentrations in outflow water and higher overall greenhouse gas fluxes from the soil surface compared with IWS. Free draining mesocosms sometimes had significantly higher nitrous oxide emissions, particularly after induced drought periods. These results suggest that stormwater basins with IWS have the potential to enhance nitrogen removal while minimizing biological greenhouse gas emissions compared with other stormwater basin drainage configurations.

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在雨水处理中,内部储水作为提高氮潴留和减少温室气体排放的手段
内部储水(IWS)作为雨水控制措施的设计元素正引起人们的兴趣。它通过一个上弯管或升高的地下排水管道来实现,在饱和条件下形成一个地下储存区,有利于通过反硝化去除氮。然而,由于地下氧化还原条件的变化,IWS可能会改变微生物产生的温室气体的排放。这些温室气体包括二氧化碳、甲烷和一氧化二氮。我们使用模拟自由排水、IWS和完全饱和雨水处理盆地的中观生态系统来研究这些生物地球化学动力学。在一系列模拟风暴事件中,我们量化了氮的去除、流出的溶解气体浓度和表层土壤温室气体的排放。IWS和完全饱和的中生态系统对硝酸盐的还原效果最好,尽管完全饱和的中生态系统输出了其他形式的氮。在温室气体排放方面,与IWS相比,完全饱和的中生态系统出水甲烷浓度最高,土壤表面温室气体总通量也更高。自由排水的生态系统有时会显著增加一氧化二氮的排放量,特别是在诱发干旱期之后。这些结果表明,与其他雨水流域排水配置相比,具有IWS的雨水流域具有增强氮去除的潜力,同时最大限度地减少生物温室气体排放。
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