Department of Biological Sciences, Idaho State University, Pocatello, ID, 83209, USA.
Environ Manage. 2020 Jan;65(1):32-45. doi: 10.1007/s00267-019-01227-x. Epub 2019 Nov 24.
Constructed stormwater wetlands (CSWs) are used to address contaminants in urban stormwater such as nitrogen (N) and phosphorus (P), but their performance is variable. Ephemeral CSWs tend to be less effective than perennial CSWs at removing N and P. We asked: How does wetland vegetation and sediment affect nutrient cycling/release from sediment and vegetation in ephemeral CSWs? We focused on two ephemeral urban CSWs in Pocatello, ID, USA, one densely vegetated and the other nearly bare. We rewetted intact cores of dry wetland sediments and, separately, senesced vegetation for 1 week at the end of the summer dry period to assess whether wetland sediments and vegetation acted as sources or sinks of N and P. For both CSWs, there was a pulse of nutrients immediately following rewetting, but the magnitude of that pulse and subsequent changes in nutrient concentrations suggest different processes dominate at each wetland, driven by differences in wetland vegetation and associated sediment characteristics. There was evidence of denitrification between and during events at the vegetated wetland, but larger fluxes of P at this site suggests a tradeoff between denitrification and P release. While the experimental results suggested specific biogeochemical controls, CSW nutrient concentrations during three events were more dynamic and suggested more biogeochemical complexity than that represented in our experiment, both within events and seasonally. Ephemeral CSWs may create unique biogeochemical conditions and require careful design to ensure N and P retention. Managers will also need to consider whether perennial water sources would improve CSW function.
人工建造的雨水湿地(CSWs)用于解决城市雨水中的污染物,如氮(N)和磷(P),但其性能存在差异。短暂性 CSWs 在去除 N 和 P 方面的效果往往不如永久性 CSWs。我们想知道:湿地植被和沉积物如何影响短暂性 CSWs 中沉积物和植被中的养分循环/释放?我们专注于美国爱达荷州波卡特洛的两个短暂性城市 CSWs,一个植被茂密,另一个几乎光秃秃的。我们在夏季干旱末期,将干燥湿地沉积物的完整核心和衰老的植被分别重新湿润了 1 周,以评估湿地沉积物和植被是否是 N 和 P 的源或汇。对于这两个 CSWs,在重新湿润后立即出现了养分脉冲,但脉冲的幅度以及随后养分浓度的变化表明,由于湿地植被和相关沉积物特征的不同,不同湿地中主导的过程也不同。在植被湿地中,在事件之间和期间都有反硝化作用的证据,但在这个地点,P 的通量更大,这表明反硝化作用和 P 释放之间存在权衡。虽然实验结果表明存在特定的生物地球化学控制,但在三个事件中 CSW 的养分浓度比我们实验中更具动态性和生物地球化学复杂性,无论是在事件内还是季节性内。短暂性 CSWs 可能会产生独特的生物地球化学条件,需要精心设计以确保 N 和 P 的保留。管理者还需要考虑永久性水源是否会提高 CSW 的功能。