For a Newtonian fluid, write , where is the rate-of-strain tensor. The Stokes equation without body force gives . Since the stress tensor is symmetric, its contraction with the antisymmetric part of the velocity gradient is zero. ThusThe divergence theorem proves the boundary-work identityFor an incompressible flow, , so is precisely the viscous dissipation.
Apply this identity to the particle-free volume and then to the fluid outside the added particle. On the rigid particle, the velocity has the form . Its contribution to the boundary work is , which vanishes because the particle is force-free and torque-free. The outer velocity is unchanged. Subtracting the two boundary-work identities therefore givesTo move this expression to the particle surface, apply the Lorentz reciprocal theorem to and in the punctured fluid domain. For completeness, its local proof isOn the outer boundary . Let be the particle-outward normal, opposite to the fluid-outward normal there. Integrating the preceding divergence identity givesThis expression includes the removal of the original fluid inside the particle; that removal must not be counted separately again.
For a sphere in a uniform straining Stokes flow, is symmetric and trace free, and . Symmetry gives zero rigid translation and rotation. Put and . Use the Unscaled Papkovich–Neuber representation printed on the paper, with the decaying harmonic potentialsTheir harmonicity follows from and from being a trace-free second derivative of . Direct differentiation givesAt , the no-slip boundary condition requires . Matching the independent and terms fixes and . The disturbance velocity and pressure are consequentlyThe pressure follows from . The disturbance decays, the total velocity vanishes at the sphere, and the harmonic representation verifies the Stokes equation. The boundary traction has zero total force by odd symmetry, and zero total torque because is symmetric, confirming the assumed force-free and torque-free motion.
At the sphere , so the extra dissipation due to a rigid inclusion becomes . Contracting the supplied total stress tensor with cancels its terms proportional to , leaving . ThusUsing proves the single-sphere dissipation increaseOne may perform the comparison in a large bounded vessel with prescribed straining velocity and then take its size to infinity; the given near-sphere approximation makes this limit compatible with the fixed-outer-velocity definition of .
The sphere number density is . Neglecting hydrodynamic interactions, the additional viscous dissipation per unit volume is . Adding the particle-free value givesThis is the Einstein viscosity formula for a dilute suspension, to first order in the particle volume fraction.
Articles by others on the same topic
There are currently no matching articles.