Stratification and its consequences in two constructed urban stormwater wetlands

• Published in: The Science of the total environment Vol. 872; p. 162179
• Main Authors: Ahmed, Sherif S., Zhang, Wenming, Loewen, Mark R., Zhu, David Z., Ghobrial, Tadros R., Mahmood, Khizar, van Duin, Bert
• Format: Journal Article
• Language: English
• Published: Netherlands Elsevier B.V 10.05.2023
• Subjects: Aquatic vegetation; Hydrodynamics; Physical processes; Stormwater; Stratification; Water quality; Wetlands; RR; vw; ρ; Physical processes; I; DO; Ta; ρo; Wetlands; R; S; T; W; Stormwater; HWL; Stratification; Vs; Aquatic vegetation; Ts; Twc; NWL; uw; d; h; Hydrodynamics; VE; η; Water quality; VN; z; RO
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2023.162179

Stratification in constructed urban stormwater wetlands is one of the fundamental physical processes that affect hydrodynamics, transport and fate of stormwater pollutants. Adverse effects of stratification include decreasing pollutant retention capacity, causing the water at lower depths to become anoxic, degrading water quality and increasing stress on the downstream aquatic communities. The current study reports on a comprehensive field monitoring program of stratification and hydrodynamics in two ice-free seasons (May – October) in two constructed urban stormwater wetlands in Calgary, Canada, with different inlet, outlet, morphometric and vegetation designs. Despite their small sizes of 0.5 and 1.2 ha and shallow water depths of 0.8 m, stratification was strong and persistent in the wetlands. The response of stratification and mixing to atmospheric forcings (e.g., air temperature, atmospheric instability, rainfall depth, wind speed) and the impact of design characteristics (inlet/outlet design, water depth, surface area and aquatic vegetation) were examined and discussed. Thermal stratification, defined as a vertical temperature gradient >1 °C/m, was found to be significantly higher (up to ten times) near the inlets and last longer (up to twice) than in the main cells and the outlet basins due to the relatively cold summer inflows. The wetland with twice the permanent water volume and surface area and half the length-to-width ratio had denser submerged aquatic vegetation, higher (by up to 2 °C) water temperature and more severe (up to eight times) thermal stratification. Strong densimetric stratification and low wind stress on the water surface caused hypoxic conditions near the bed, potentially adversely affecting water quality and downstream aquatic communities. [Display omitted] •A 2-year field monitoring study in 2 nearby 0.8 m deep wetlands in Calgary, Canada•Vertical temperature gradient >1 °C/m persisted for two-thirds of May–October•Surface velocities scaling at 0.3 % of the wind speed did not induce mixing•Prolonged stratifications in July & August caused hypoxia near the bed•Surface area & vegetation cause notable differences in temperature & stratification