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应用 N 标记方法估算生物滞留系统中的氮归宿和总转化。

Estimating nitrogen fates and gross transformations in bioretention systems with applications of N labeling methods.

机构信息

School of Atmospheric Sciences, Sun Yat-sen University, Key Laboratory for Tropical Atmosphere-Ocean System, Ministry of Education, Zhuhai, 519082, China; Key Laboratory for Urban Habitat Environmental Science and Technology, School of Environment and Energy, Peking University Shenzhen Graduate School, 518055, Shenzhen, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China.

Key Laboratory for Urban Habitat Environmental Science and Technology, School of Environment and Energy, Peking University Shenzhen Graduate School, 518055, Shenzhen, China; Department of Civil and Environmental Engineering, National University of Singapore, 1 Engineering Drive 3, Singapore, 117580, Singapore.

出版信息

Chemosphere. 2021 May;270:129462. doi: 10.1016/j.chemosphere.2020.129462. Epub 2020 Dec 28.

Abstract

Two batches of NH and NO labeling experiments were conducted to understand the complex nitrogen (N) fates and transformations in bioretention systems, respectively. The fates of NH were first traced in six bioretention systems with different wet-dry regimes and submerged zone settings during four months, indicating: (1) N was mainly leached during the second storm events following the NH addition during the first storm events, suggesting nitrification during the dry period; (2) the main NH fates after four-month exposure were: soil media 59.6%-80.0%, outflow 5.3%-16.4%, plants 2.3%-8.9%, denitrification losses 0-28.4%; (3) longer antecedent dry weather period and submerged zone could help alleviate outflow NO leaching. The occurrence time, positions and rates of major N transformation processes were later examined by the NO labeling experiment in a bioretention system over an 8 d wet-dry cycle, indicating: (1) during the brief wet period, hydraulic mixing of "old" water and "new" inflow mainly occurred; (2) during the subsequent dry period, gross rates of nitrification, denitrification and mineralization showed "pulse effects", i.e. peaking at 24-48 h and decreasing significantly within 72 h; (3) denitrification became more dynamic with soil media depth, especially in submerged zone. This study evidenced the feasibility of N labelling method in studying N dynamics in bioretention systems and would inform future engineering and stormwater management practices.

摘要

本研究通过两批次 NH 和 NO 示踪实验,分别研究了城市生物滞留系统中复杂的氮(N)去向和转化。在为期四个月的时间里,通过对六个具有不同干湿交替期和淹没区设置的生物滞留系统进行 NH 示踪实验,发现:(1)NH 主要在首次暴雨事件后第二次暴雨事件中淋溶损失,表明干湿交替期存在硝化作用;(2)暴露四个月后,NH 的主要去向为:土壤介质 59.6%-80.0%、出流 5.3%-16.4%、植物 2.3%-8.9%、反硝化损失 0-28.4%;(3)较长的前期干燥天气期和淹没区有助于减少出流出硝态氮淋溶。随后,通过在一个生物滞留系统中进行为期 8 天的干湿循环的 NO 示踪实验,进一步研究了主要氮转化过程的发生时间、位置和速率,结果表明:(1)在短暂的湿期,主要发生“旧”水和“新”入流水的水力混合;(2)在随后的干期,硝化、反硝化和矿化的总速率呈现“脉冲效应”,即在 24-48 小时达到峰值,72 小时内显著下降;(3)反硝化作用随土壤介质深度的增加而变得更加活跃,特别是在淹没区。本研究证明了 N 示踪方法在研究生物滞留系统中 N 动态变化方面的可行性,并为未来的工程和雨水管理实践提供了信息。

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