3 years ago

The effects of initial soil moisture conditions on swale flow hydrographs

Maria Viklander, Hendrik Rujner, Anna-Maria Perttu, Jiri Marsalek, Günther Leonhardt
The effects of soil water content (SWC) on the formation of runoff in grass swales draining into a storm sewer system were studied in two 30-m test swales with trapezoidal cross-sections. Swale 1 was built in a loamy fine-sand soil, on a slope of 1.5% and Swale 2 was built in a sandy loam soil, on a slope of 0.7%. In experimental runs, the swales were irrigated with two flow rates reproducing runoff from block rainfalls with intensities approximately corresponding to two-month and three-year events. Runoff experiments were conducted for SWCini (initial SWC) ranging from 0.18 to 0.43 m3m-3. For low SWCini, the runoff volume was greatly reduced by up to 82%, but at high SWCini, the volume reduction was as low as 15%. The relative swale flow volume reductions decreased with increasing SWCini and, for the conditions studied, indicated a transition of the dominating swale functions from runoff dissipation to conveyance. Runoff flow peaks were reduced proportionally to the flow volume reductions, in the range from 4-55%. The swale outflow hydrograph lag-times varied from 5 to 15 minutes, with the high values corresponding to low SWCini. Analysis of swale inflow/outflow hydrographs for high SWCini allowed estimations of the saturated hydraulic conductivities as 3.27 and 4.84 cm/h, in Swales 1 and 2, respectively. Such estimates differed from averages (N=9) of double-ring infiltrometer measurements (9.41 and 1.78 cm/h, respectively). Irregularities in swale bottom slopes created bottom surface depression storage of 0.35 and 0.61 m3, for Swales 1 and 2, respectively, and functioned similarly as check-berms contributing to runoff attenuation. The experimental findings offer implications for drainage swale planning and design: (i) SWCini strongly affect swale functioning in runoff dissipation and conveyance during the early phase of runoff, which is particularly important for design storms and their antecedent moisture conditions, and (ii) concerning the longevity of swale operation, Swale 1 remains fully functional even after almost 60 years of operation, as judged from its attractive appearance, good infiltration rates (3.27cm/h), and high flow capacity.

Publisher URL: http://onlinelibrary.wiley.com/resolve/doi

DOI: 10.1002/hyp.11446

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