The recession flow analysis of Brutsaert and Nieber  extended by Troch et al.  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.
|Number of pages||7|
|Journal||Water Resources Research|
|Publication status||Published - Jul 1998|