A confined aquifer has a thickness of l 0.0 m and a transmissivity of 1.30 × 10-3 m2/sec. When a 30-cm-diameter well is pumped at the rate of 30 m3 /hr, the drawdown of the piezometric surface at an observation well 30 m away is 9.60 m when it is not impacted by an aquifer boundary. If an identical well is installed in the same aquifer but located 30 m from a fully penetrating impermeable boundary, determine the drawdown at the boundary and at the well.