Abstract:
Hydrographs were recorded at three discharge stations at a small alluvial stream during the summers of 1997 and 1998. A method of analysis was set up so that the temporal variations in discharge resulting from natural hydrological processes can be distinguished from the influence from ground water being periodically abstracted approximately 60m from the stream. Thus, evapotranspiration from the riparian zone resulted in diurnal variations in streamflow with maximum amplitude of 3-5l/s, whereas heavy rainfall resulted in intense short-term surface/subsurface flow from the riparian zone. The magnitude of peak-flow was of the order of 2-3 times baseflow and such events typically disturbed the hydrograph for one to three days. Baseflow increased from about 35l/s to about 70l/s over the studied reach, but when ground water was abstracted at rates of about 15l/s this resulted in a reduction in discharge. Within 4-8 days the reduction stabilized at about 4l/s and at 5-7l/s, respectively, at discharge stations 140 and 350m downstream of the well site. Predictions made by the analytical depletion model by [Ground Water, 37 (1999) 98] using the values of transmissivity and conductance of the streambed estimated by [Ground Water, 40 (2002) 437] by drawdown analysis compare reasonably well to the observed reduction of streamflow.
