Step 1: Trace the path water takes to reach the water table.
Precipitation first infiltrates into the topsoil, entering the unsaturated zone.
Step 2: Follow the water downward.
From there it percolates further down through the soil and rock until it reaches the saturated zone, adding to the groundwater store.
Step 3: Rule out the other processes.
Surface runoff and interception keep water on or near the surface, and evapotranspiration returns water to the atmosphere, so none of these add to groundwater.
\[ \boxed{\text{Infiltration and percolation}} \]