Department of Civil and Mineral Engineering, University of Toronto, 35 St George St, Toronto, ON M5S 1A4, Canada.
Ecohydrology Research Group, Water Institute and Department of Earth & Environmental Sciences, University of Waterloo, 200 University Avenue West, Waterloo, ON N2L 3G1, Canada.
Sci Total Environ. 2019 Feb 1;649:749-759. doi: 10.1016/j.scitotenv.2018.08.366. Epub 2018 Aug 27.
Bioretention cells are a popular control strategy for stormwater volume and quality, but their efficiency for water infiltration and nutrient removal under cold climate conditions has been poorly studied. In this work, soil cores were collected from an active bioretention cell containing engineered soil material amended with a phosphate sorbent medium. The cores were used in laboratory column experiments conducted to obtain a detailed characterization of the soil's bioretention performance during six consecutive freeze-thaw cycles (FTCs, from -10 to +10 °C). At the start of each FTC, the experimental column undergoing the FTCs and a control column kept at room temperature were supplied with a solution containing 25 mg/L of bromide, nitrate and phosphate. Water saturated conditions were established to mimic the presence of an internal water storage zone to support anaerobic nitrate removal. At the end of each FTC, the pore solution was allowed to drain from the columns. The results indicate that the FTCs enhanced the infiltration efficiency of the soil: with each successive cycle the drainage rate increased in the experimental column. Freezing and thawing also increased the saturated hydraulic conductivity of the bioretention soil. X-ray tomography imaging identified a key role of macro-pore formation in maintaining high infiltration rates. Both aqueous nitrate and phosphate supplied to the columns were nearly completely removed from solution. Sufficiently long retention times and the presence of the internal water storage zone promoted anaerobic nitrate elimination despite the low temperatures. Dissolved phosphate was efficiently trapped at all depths in the soil columns, with ≤2% of the added stormwater phosphate recovered in the drainage effluent. These findings imply that, when designed properly, bioretention cells can support high infiltration rates and mitigate nutrient pollution in cold climates.
生物滞留池是一种用于控制雨水径流量和水质的流行控制策略,但在寒冷气候条件下,其对水渗透和养分去除的效率研究甚少。在这项工作中,从一个含有工程土壤材料的活性生物滞留池中采集了土壤芯,该土壤材料中添加了磷酸盐吸附剂介质。这些芯被用于实验室柱实验中,以在六个连续的冻融循环(FTCs,从-10°C 到+10°C)期间对土壤的生物滞留性能进行详细表征。在每个 FTC 开始时,正在进行 FTC 的实验柱和保持在室温下的对照柱都用含有 25mg/L 溴化物、硝酸盐和磷酸盐的溶液供应。建立水饱和条件以模拟内部储水层的存在,以支持厌氧硝酸盐去除。在每个 FTC 结束时,允许从柱中排出孔隙溶液。结果表明,FTCs 提高了土壤的渗透效率:随着每个连续的循环,实验柱中的排水速率增加。冻结和融化还增加了生物滞留土壤的饱和水力传导率。X 射线断层扫描成像确定了大孔形成在保持高渗透速率方面的关键作用。向柱中供应的水合硝酸盐和磷酸盐几乎都从溶液中完全去除。尽管温度较低,但足够长的保留时间和内部储水层的存在促进了厌氧硝酸盐的消除。溶解的磷酸盐在土壤柱的所有深度都被有效地捕获,添加的雨水中只有≤2%的磷酸盐在排水废水中回收。这些发现表明,在设计合理的情况下,生物滞留池可以在寒冷气候下支持高渗透速率并减轻营养物污染。