Volume conservation states that the volume of incompressible material can change only through boundary fluxes or specified sources and sinks. In a one-dimensional shallow layer of depth h and depth-averaged speed u, it has the form ht+(hu)x=s.
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- Confined plume with compensating return flow
- Entraining shallow-water current in a triangular channel
- Filling-box first front
- Multiple-plume displacement ventilation
- No steady displacement layer without ambient supply
- Particle-laden current with suction
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- Prismatic-channel shallow water equations
- Prismatic triangular-channel shallow water equations
- Steady depositing gravity current
- Triangular-channel shallow water equations
- U-tube differential manometer
- Variable-section channel characteristics
- Variable-width shallow-water characteristics
- Vertical imbibition under a draining liquid layer
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