To accurately calculate and interpret mass flux, converting the velocity field to the appropriate coordinate system (e.g., cylindrical) is crucial, especially when dealing with surfaces defined in that system. The mass flux value itself then provides a quantitative measure of the net rate of mass flow across a surface, with a positive flux indicating outflow, negative indicating inflow, and zero signifying flow along the surface rather than through it.
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The first and most critical step was converting the Cartesian velocity field into cylindrical coordinates. This was essential because the surfaces given in the problem were defined cylindrically. Failing to do this would have made the calculations much more complex, if not impossible. The simplified form of the velocity field, $v=\frac{v_0}{L}\left(\rho e_\phi+L e_z\right)$, revealed the true nature of the flow: a combination of rotational motion ( $e_\phi$ ) and a constant vertical flow ( $e_z$ ).
The value of the mass flux, $\Phi$, represents the net rate of mass flow across a given surface. A positive flux means fluid is flowing out of the volume, a negative flux means fluid is flowing in, and a zero flux means there is no net flow across the surface.
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