Abstract
The recession flow analysis of Brutsaert and Nieber [1977] extended by Troch et al. [1993] to estimate aquifer parameters (saturated hydraulic conductivity and mean aquifer depth) is examined by means of a numerical model. It is found to be reliable for the estimation of the catchment-scale saturated hydraulic conductivity and mean aquifer depth. Increasing the complexity of the synthetic watershed had no impact on the accuracy of the estimated parameters.
| Original language | English |
|---|---|
| Pages (from-to) | 1851-1857 |
| Number of pages | 7 |
| Journal | Water Resources Research |
| Volume | 34 |
| Issue number | 7 |
| Publication status | Published - Jul 1998 |
| Externally published | Yes |