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Tile drainage also accounted for 47% of watershed discharge and was seasonally variable.
Results showed that tile discharge accounted for 56% of annual watershed discharge over the 8-year study.
Study results indicate that tile drainage is the primary factor controlling watershed discharge and N, especially NO3 N, export in systematically tile-drained agricultural headwater watersheds.
The objective of this study was to ascertain seasonal and annual contributions of tile drainage to watershed discharge and N loading.
While the metals loads were quantifiable from the CSOs, the loads associated with the upper watershed discharge were greater, for example, by a factor of 3 to 18 times for the design storms.
With these benefits in mind, the Data Uncertainty Estimation Tool for Hydrology and Water Quality (DUET-H/WQ) was developed from an existing uncertainty estimation framework for small watershed discharge, sediment, and N and P data.
Similar(53)
If, at the watershed scale, basin discharge or recharge boundary conditions are needed, then this study suggests some local calibration is necessary.
Both watersheds discharged into the same lagoon at M2 and M4.
As a result of calibration, predicted basin discharge closely matches measured data for validation watersheds.
Estimates of mean annual watershed sediment discharge, derived from long-term measurements of suspended-sediment concentration and streamflow, often are not available at locations of interest.
Recently, the watershed stream discharge has increased, causing flooding (Kebede et al. 2014).
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