Classical Stochastic Processes¶
The generalized transport coefficient framework subsumes several classical stochastic models as special cases. This section catalogs these limits, following PNAS 2024 SI Section 4 (Eqs. S-108 through S-127), and shows how each maps onto the power-law parameterization used by the heterodyne package.
Wiener Process (Standard Diffusion)¶
The Wiener process describes free Brownian motion with a constant diffusion coefficient \(D\). The transport coefficient is:
and the internal field correlation is:
This is the simplest case: the position variance grows linearly in time, \(\mathrm{Var}\!\left[x(t)\right] = \int_0^t J(t')\, dt'\), and the correlation decays monotonically with the integrated transport.
Power-law mapping: \(\alpha = 0\), \(D_0 = 2D\), \(D_\mathrm{offset} = 0\).
Ornstein-Uhlenbeck Process¶
The Ornstein-Uhlenbeck (OU) process models diffusion in a harmonic potential with restoring rate \(\gamma\):
At short times (\(t \ll 1/\gamma\)), the particle is ballistic and \(J(t) \approx 2D\gamma^2 t^2\). At long times (\(t \gg 1/\gamma\)), the velocity decorrelates and \(J(t) \to 2D\), recovering Fickian diffusion.
The OU process is not exactly representable by the power-law parameterization, but for time windows much longer than \(1/\gamma\) it is well approximated by \(\alpha = 0\).
Brownian Oscillator¶
The Brownian oscillator describes a particle in a harmonic potential with natural frequency \(\omega_0\) and damping rate \(\gamma\). It exhibits two regimes:
Overdamped (\(\gamma > 2\omega_0\)):
where \(\Omega = \sqrt{(\gamma/2)^2 - \omega_0^2}\).
Underdamped (\(\gamma < 2\omega_0\)):
where \(\omega = \sqrt{\omega_0^2 - (\gamma/2)^2}\).
In both cases, \(J(t) \to 2D\) at long times. The underdamped case exhibits oscillatory transients in \(J(t)\) that can produce non-monotonic correlation decay at short lag times.
Advection-Diffusion¶
The advection-diffusion model combines Brownian diffusion with a constant drift velocity \(v_0\). Using the internal/external factorization:
The first factor is the diffusive decay (transport integral); the second is the advective phase shift (velocity integral). In a homodyne measurement, the phase vanishes under the modulus squared:
so the velocity is invisible. In a heterodyne measurement, the velocity produces observable oscillations in the cross-correlation (see Heterodyne Scattering Model).
Power-law mapping: \(\alpha = 0\), \(D_0 = 2D\), \(D_\mathrm{offset} = 0\), with velocity \(v(t) = v_0\) (i.e., \(\beta_v = 0\), \(v_\mathrm{offset} = v_0\)).
Power-Law Transport¶
The general power-law parameterization used in the heterodyne package (PNAS 2024 SI Eq. S-105):
This phenomenological form captures the leading-order behavior of a wide class of transport processes:
Parameters |
Model |
Physical scenario |
|---|---|---|
\(\alpha = 0,\; D_\mathrm{offset} = 0\) |
Wiener |
Free diffusion |
\(\alpha < 0\) |
Subdiffusive |
Viscoelastic confinement, crowded environments |
\(0 < \alpha < 1\) |
Weakly superdiffusive |
Persistent random walks |
\(\alpha = 1\) |
Ballistic |
Uniform acceleration |
\(D_\mathrm{offset} \neq 0\) |
Mixed |
Baseline diffusion with time-dependent correction |
The offset \(D_\mathrm{offset}\) allows the model to accommodate processes that have a finite transport rate at \(t = 0\) (e.g., a Wiener component superimposed on a power-law anomalous process).
Summary of Limits¶
Process |
\(J(t)\) |
Short-time |
Long-time |
|---|---|---|---|
Wiener |
\(2D\) |
\(2D\) |
\(2D\) |
OU |
\(2D(1-e^{-\gamma t})^2\) |
\(\sim t^2\) |
\(2D\) |
Oscillator |
(see above) |
\(\sim t^2\) |
\(2D\) |
Advection-diffusion |
\(2D\) |
\(2D\) |
\(2D\) |
Power-law |
\(D_0 t^\alpha + D_\mathrm{offset}\) |
\(D_\mathrm{offset}\) |
\(\sim t^\alpha\) |