In hydrodynamics, the Perrin friction factors are multiplicative adjustments to the translational and rotational friction of a rigid spheroid, relative to the corresponding frictions in spheres of the same volume. These friction factors were first calculated by Jean-Baptiste Perrin. These factors pertain to spheroids, which are characterized by the axial ratiop = , defined here as the axial semiaxisa divided by the equatorial semiaxis b. In prolate spheroids, the axial ratio p > 1 since the axial semiaxis is longer than the equatorial semiaxes. Conversely, in oblate spheroids, the axial ratio p < 1 since the axial semiaxis is shorter than the equatorial semiaxes. Finally, in spheres, the axial ratio p = 1, since all three semiaxes are equal in length. The formulae presented below assume "stick" boundary conditions, i.e., it is assumed that the velocity of the fluid is zero at the surface of the spheroid.
Perrin S factor
For brevity in the equations below, we define the Perrin S factor. For prolate spheroids where the parameter is defined Similarly, for oblate spheroids For spheres,, as may be shown by taking the limit for the prolate or oblate spheroids.
There are two rotational friction factors for a general spheroid, one for a rotation about the axial semiaxis and other for a rotation about one of the equatorial semiaxes. Perrin showed that for both prolate and oblate spheroids. For spheres,, as may be seen by taking the limit. These formulae may be numerically unstable when, since the numerator and denominator both go to zero into the limit. In such cases, it may be better to expand in a series, e.g., for oblate spheroids.
Time constants for rotational relaxation
The rotational friction factors are rarely observed directly. Rather, one measures the exponential rotational relaxation in response to an orienting force. The time constant for relaxation of the axial direction vector is whereas that for the equatorial direction vectors is These time constants can differ significantly when the axial ratio deviates significantly from 1, especially for prolate spheroids. Experimental methods for measuring these time constants include fluorescence anisotropy, NMR, flow birefringence and dielectric spectroscopy. It may seem paradoxical that involves. This arises because re-orientations of the axial direction vector occur through rotations about the perpendicular axes, i.e., about the equatorial axes. Similar reasoning pertains to.