Set under the assumed stationary-onset hypothesis, and let with fixed nonzero . Substitute , , and into the modal equations and plate boundary conditions.
At leading order the concentration equation is , with at both plates. Normalize its nonzero constant to . The first nonzero momentum equation is
Integrating four times and imposing all four clamped boundary conditions gives
At the next concentration order, and , so the vertical advection of the basic concentration does not yet contribute. Thus
Integration gives . The constant is an amplitude-normalization freedom; set it to zero, obtaining
There is no need to require zero depth average of this concentration eigenfunction: for a nonzero horizontal wavenumber the horizontal average is already zero.
Use and . At order , the concentration equation is
The corresponding cell-flux boundary conditions are at both plates. Integrate the equation from to zero. Its left derivative term satisfies
The terms therefore cancel. The no-slip conditions imply . Also integration by parts gives
Consequently the solvability condition is simply
since . For every fixed nonzero , the long-wave bioconvection threshold in weak stratification is therefore
The cancellation shows why does not enter this leading coefficient; neither does at stationary onset. In dimensional terms, the leading critical mean number density and volume fraction are
These assume heavier-than-fluid cells, . Exactly makes the integrated equation identically zero and corresponds to a spatially uniform change of conserved cell number, not a convective mode; the statement independent of is interpreted for nonzero long waves or their limit. This is the leading threshold within the specified long-wave, real-eigenvalue assumptions. It does not by itself rule out a different finite-wavelength or oscillatory instability outside those assumptions.