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Plane potential flows assume fluid is irrotational and incompressible, allowing description by a velocity potential function and stream function governed by Laplace's equation. These assumptions simplify complex fluid motion into manageable mathematical models for predicting flow patterns, velocity distributions, and pressure fields around hydraulic structures.

Uniform flow represents the simplest potential flow, with fluid moving in a straight line at constant velocity. Streamlines are straight, parallel, and evenly spaced, making it essential for designing canals, pipelines, and drainage systems where constant velocity aids in flow rate estimation and hydraulic design.

Source flows model groundwater recharge from injection wells, with fluid moving radially outward from a central point. Sink flows represent groundwater extraction from pumping wells, with fluid converging inward. These radially symmetric flows are modeled using flow rate parameters to represent source or sink strength in hydrology.

Free vortex flows involve particles circulating a center point without external force, creating whirlpool effects used in spillway and drainage design. Forced vortex flows are driven by external forces, rotating fluid as a rigid body, applied in sedimentation tanks and hydraulic devices for sediment separation and fluid mixing.

Flow nets combine streamlines representing fluid flow paths with equipotential lines marking equal hydraulic potential points. These perpendicular intersecting lines create grid patterns identifying pressure distributions and potential seepage paths. Careful analysis of spacing and orientation reveals erosion risks and structural weaknesses around dams and similar structures.

The stream function visualizes flow paths in potential flows, working alongside the velocity potential function to describe the complete flow field. Both functions are governed by Laplace's equation and enable engineers to estimate flow patterns, velocity distributions, and pressure fields essential for designing structures interacting with fluids.

Plane potential flows predict flow patterns and seepage paths around hydraulic structures like dams and levees, identifying areas vulnerable to water infiltration. By analyzing flow nets and velocity distributions, engineers manage water resources effectively and prevent structural weakening from uncontrolled seepage and erosion.