The dynamical-scaling hypothesis replaces all macroscopic lengths by one scale and the characteristic velocity by . Then inertial, viscous, and capillary force densities scale respectively as , , and .
Replacing domain-scale viscous stresses by a local linear drag density gives the scales and . The single-scale force model isFor a regular power-law asymptotic , , , , the two inertial-to-drag ratios scale as and . Thus drag dominates inertia at late time, and drag-capillary balance integrates to . This proves the displayed exponent and its independence of mass density. The scaling assumes a homogenized stationary network and dominant advective transport. Diffusive Ostwald ripening can have the same exponent, so its omission must be justified separately; order-parameter mobility can otherwise enter the prefactor.
Under single-length dynamical scaling of binary-fluid coarsening, mass density , dynamic viscosity and surface tension determine the displayed unique length and time scales by dimensional analysis. Writing reduces the force-density estimate to . Resistive and driving terms need opposite signed geometric coefficients. Viscous hydrodynamic coarsening has and inertial hydrodynamic coarsening has . These follow respectively from density-independent and viscosity-independent powers in . They require thin interfaces, statistically self-similar bicontinuous domains, dominant advection and no additional relevant macroscopic scales. A degeneracy in the signed inertial coefficients can invalidate the pure-power force balance without invalidating the dimensional calculation.
Balancing viscous and capillary forces gives . This regime is independent of the mass density and applies below the viscous-to-inertial crossover scale.
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