Step 1: Compare a fully penetrating well with a partial one.
A well that reaches all the way through an aquifer draws water in mostly horizontal, evenly spaced flow lines.
Step 2: Think about what changes with partial penetration.
When a well only taps part of the aquifer's thickness, water has to converge toward that shorter screened section from above and below as well as sideways.
Step 3: Describe the resulting pattern.
This mix of horizontal and vertical movement near the well creates a genuinely three-dimensional, complex flow pattern, not the simple uniform flow, reduced recharge, or zero drawdown listed in the other options.
\[ \boxed{\text{Complex flow}} \]