The equation of continuity is derived assuming the flow rate is the same everywhere. Therefore, the flow rate is the same at any two points.

where
- mass that flows past a point (kilograms)
- time interval (seconds)
Consider thin cross-sectional slices of fluid that flow past points a and b during some time interval. The mass of each slice can be replaced by the density and volume.

where
- density at a point (kilograms / meter3)
- volume that flows past a point (meters3)
The volume of the slice equals the cross-sectional area times the distance that the slice travels during the time interval.

where
- cross-sectional area at a point (meter2)
- distance traveled (meters)
The ratio of distance over time is simply the velocity. This gives the equation of continuity.

where
- velocity past a point (meters / second)