The Laplacian and the added drag term in the Brinkman equation must have the same dimensions. ThereforeThe length is a hydrodynamic screening length. When the viscous coefficients are identical in the two terms, the corresponding permeability is .
Scale time by , length by , velocity by , pressure by , and streamfunction by . Write , , and drop stars from dimensionless coordinates. The surface is and its material velocity in the sheet frame is . The no-slip boundary condition is thereforeThe stationary matrix identifies a preferred frame. In the sheet frame it translates with , so matrix-relative Brinkman velocity gives the consistent equationsEquivalently one may keep the printed right-hand side after defining ; then the far-field pressure has the gradient needed to balance that term. Using the printed equation with a uniform far-field flow and no such adjustment is inconsistent. The distinction first matters at second order, since the first-order swimming speed is zero. We solve the upper half-space; the lower half-space is its reflected counterpart.
Taking the curl of the Brinkman equation eliminates pressure and the constant matrix velocity. With and vorticity , the Brinkman swimming sheet equation isThe surface conditions are conditions on partial derivatives evaluated on the moving boundary:At infinity, and . The derivative of along the surface also equals , because there, so a convenient gauge has . Decaying perturbations and the force-free condition determine the swimming solution.
Expand and . The screened first-order transverse sheet flow has . Set . The two decaying roots of the Brinkman swimming sheet operator are and , and , selectThe physical first-order flow is in scaled coordinates. The dimensionless first-order pressure, determined from momentum balance, isAlthough the expression for appears singular at , its continuous limit is , the ordinary transverse mode of a Taylor swimming sheet.
A Taylor expansion of the tangential no-slip boundary condition gives . Since ,For matrix-relative Brinkman velocity, the mean second-order tangential flow isThe mean tangential traction has no first-order geometric remainder: at the surface and , so the mean displaced-boundary and tilted-normal corrections cancel. Thus the force-free condition gives , hence . In the limit boundedness likewise excludes mean shear. The swimming speed of a Brinkman sheet is thereforeIt is larger than the simple-fluid speed by for fixed waveform and frequency. The matrix offers a reaction structure for the transverse stroke and more strongly confines the induced motion; it acts as a footing against which the wave pushes. This is a prescribed-stroke comparison, not a guarantee at fixed motor power. The small-amplitude expansion is at fixed ; a large- use also needs to control variation across the displaced boundary.
At the undeformed boundary, the screened first-order transverse sheet flow has and . Hence the normal stress is . The sheet does work on the upper fluid at rate , where points from the sheet into that fluid. To second order only the first-order normal velocity and stress are needed. The power of a Brinkman sheet per projected area on one side isFor fluid on both sides, double this answer. At the one-sided power is , so the fixed-stroke cost increases by . The mechanical energy supplied to the fluid accounts for both viscous dissipation and work against the matrix drag; the stress still has the printed Newtonian form. Enhanced speed therefore comes with increased energetic cost.
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