Fluid Mechanics, Fourth Edition

The coordinates are (R, ?,x), where ? is theazimuthal angle (see Figure 3.1b, where ? is used instead of ?). The equations are presented assuming ? is a scalar, and
where i R, i ?, and i x are the local unit vectors at a point.
Gradient of a scalar
Laplacian of a scalar
Divergence of a vector
Curl of a vector
Laplacian of a vector
Strain rate and viscous stress (for incompressible form ? ij = 2 ?e ij)
Vorticity ( ? = ? u)
Equation of continuity
Navier-Stokes equations with constant ? and ?, and no body force
where
The plane polar coordinates are (r, ?), where r is the distance from the origin (Figure 3.1a). The equations for plane polar coordinates can be obtained from those of the cylindrical coordinates presented in Section B1, replacing R by r and suppressing all components and derivatives in the axial direction x. Some of the expressions are repeated here because of their frequent occurrence.
Strain rate and viscous stress (for incompressible form ? ij = 2 ?e ij)
Vorticity
Equation of continuity
Navier-Stokes equations with constant ? and ?, and no body force
where
The spherical polar coordinates used are (r, ?, ?), where ? is the azimuthal angle (Figure 3.1c).