The Stokes–Einstein relation gives the translational diffusion coefficientat . For isotropic three-dimensional Brownian motion, the mean squared displacement is . Thus after one hour the root mean square displacement isThe phrase “on average” needs a convention: the mean displacement vector is zero; the mean displacement magnitude of three-dimensional Brownian motion is , obtained by integrating the three-dimensional Gaussian distribution. These are displacements, not the total microscopic path length. The estimate assumes dilute unconfined water, a spherical hydrodynamic radius and constant temperature.
For a spherical micelle with tails, core radius , molecular tail volume and head-group area , volume and surface counting give and . Consequently . A tail cannot span a core radius larger than its maximum length , so the amphiphile packing parameter condition isThis is a minimum area, not a maximum. The printed request reverses the geometric inequality. The limiting value corresponds to fully extended tails with ; larger head groups permit smaller spherical aggregates in this simple packing argument. The supplied data alone impose no finite maximum head-group area, and geometry alone does not guarantee thermodynamic micelle formation.
In the planar Debye–Hückel approximation, a surface potential decays as , with at fixed temperature and solvent permittivity; is the ionic strength. For a monovalent salt, reducing its concentration by ten reduces by . Calibrating the first decay from the supplied potential ratio, and assuming unchanged , givesHere the printed meV unit is interpreted as the electrostatic potential energy of a singly charged probe; the same ratio calculation applies to potentials in mV.
This numerical answer uses an effective exponential decay calibrated from the data. The inferred initial Debye length is , whereas the standard dilute aqueous-electrolyte expression at room temperature gives about for monovalent salt. The numbers therefore are not consistent with that absolute ideal-electrolyte model. Moreover a spherical colloid has an additional radius-dependent geometric factor, and its surface potential need not remain constant when salt is changed. Without a surface boundary condition and geometry, the new potential is not uniquely specified beyond the stated planar, fixed-potential approximation.
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