Infiltration capacity in urban areas undergoing frequent snow and freeze-thaw cycles: Implications on sustainable urban drainage systems

Sustainable Urban Drainage Systems (SuDS) promote environmental protection and climate resilience. SuDS implementation in cold climates faces concerns of impaired hydrological function due to infiltration-reducing frost. The goal of this research was to assess the seasonal variations in infiltration and how different surface covers prevalent in and near coastal cities respond to frequent rain-on-snow and freeze-thaw cycles. A total of 28 constant head infiltration measurements were conducted over a period of 28 months in Urridaholt in Gardabaer, Iceland (64. 4'18.46 '' N, 21 degrees 54'37.11 '' W) in a grass swale, lupine, and barren terrains. All test locations exhibited infiltration-inhibiting frost in winter, whose severity increased with frequent snow and freeze-thaw cycles. The grass swale resisted structural deformations resulting from frost, which was attributed to the high near-surface porosity within the intertwined root layer and the high drainage capacity of the underlying soil. The sparsely vegetated lupine and the barren area experienced severe frost heaving and cracking, and soil structural collapse which led to bypass flow upon thawing. The non-vegetated site had 30 to 50 times lower infiltration during winter (19 mm h(-1)) compared to the grass swale and lupine field (630- and 890-mm h(-1), respectively), and twenty times lower during summer and fall (45 mm h(-1) vs. similar to 1000 mm h(-1)). The study concludes that frequent warming and cooling renders soils particularly vulnerable to frost. Vegetation plays an instrumental role in maintaining the hydrological functions of SuDS in winter. Therefore, the greening of urban centers is an important step towards climate resiliency. Plant selection and SuDS design criteria need to account for cold climate hydrological performance. In that regard, plants that limit sunlight and fully shed their vegetation in winter, such as the invasive lupine, can potentially contribute to frost formation and increase runoff generation.

Automated summary

This research aims to assess the impact of different surface covers on infiltration in cold climates. The results indicate that only grass swales can effectively resist frost, while sparsely vegetated lupine fields and barren areas experience severe structural deformations and soil collapse. The grass swale and lupine field exhibit much higher infiltration compared to the non-vegetated site, highlighting the crucial role of vegetation in maintaining hydrological functions in winter.