THEORETICAL DRAWDOWN OF A HORIZONTAL WATER WELL WITHIN A DEEP CONFINED CLASTIC AQUIFER
Several mathematical formulae for the determination of drawdown for a partially penetrating well in a confined aquifer were analyzed to see if they could be applied to a horizontal well. Hantushs method of drawdown for a collecting well was also considered. A small-scale physical model representing a deep sand aquifer confined by clay was constructed to support the mathematical analysis. The model includes small fully penetrating monitoring wells placed around the pumping well to monitor the potentiometric surface changes. Another small-scale model with partially penetrating monitoring wells was used to compare the results from the first model. The simulated aquifer was pressurized to observe the changes in the potentiometric surface while the horizontal well was pumped at a constant rate. Data were then applied using the Theis method to show the change in drawdown with respect to time and compared to the Theis curve for a vertical partially penetrating well.