The most common method measures the time for draining of a specific volume of a solution through a capillary in response to gravity. This phenomenon is described by Poiseuille's equation.
v = pi Pr4/ 8 eta l
etarel = eta / eta0 = l rho / l0 rho0
Often the solutions are so dilute that the ratio of the densities can be taken to be 1. The concentration dependence of etarel is
etarel = 1 + [eta]c + kc2 + ...
For sufficiently dilute solutions, the intrinsic viscosity, [eta], of polymers without strong interactions is obtained via linear extrapolation, PC Fig. 10.12, suggested by
(etarel - 1)/c = etasp/c = [eta] + kc
where etasp is the specific viscosity. (This plot is decidedly nonlinear when a strongly ionized polyelectrolyte is diluted with water, F Fig. 146, due to expansion of the polymer as the counterions are diluted.) Somewhat different forms were suggested by Huggins
etasp/c = [eta] + k'[eta]2c
and Kraemer
(ln etarel)/c = [eta] + k"[eta]2c
The constants in the last two equations are related by k" = k' - 1/2.
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