Static and dynamic correlations
True colloidal systems can be complex:
Their theoretical description focuses on essential ingredients.
A simplifying assumption is that the potential energy of a collection of colloids is purely pairwise
U_N\left(\mathbf{r}^N\right)=\sum_{i=1}^{N-1} \sum_{j=i+1}^N V\left(r_{i j}\right)=\frac{1}{2} \sum_{i \neq j} V\left(r_{i j}\right)
where V(r_{ij}) is the pairwise, radial interaction potential that only depends on the distance between particle centres r_{ij} = |\mathbf{r}_i-\mathbf{r}_j|.
Some examples of non-pairwise situations:

You have already seen such correlations in other contexts (Ising model, lattice gas).
The key pair correlation is the real space radial distribution function:
g(r)=\frac{1}{4\pi r^2\rho N}\left\langle\sum_{i=1}^N \sum_{j \neq i} \delta\left(\left|\mathbf{r}_i-\mathbf{r}_j\right|-r\right)\right\rangle
The radial distribution function, algorithmic interpretation: at a distance r, we count the number of particle centres within a slice of width dr and then normalise.
The radial distribution function g(r) is related to the average local density at a distance r from a reference particle:
To formally derive this, consider a system of N particles in volume V with average density \rho = N/V. The local density at a distance r from a reference particle is the number of particles in a shell of radius r divided by the shell volume 4\pi r^2 dr. Averaging over the N reference particles, \langle \rho(r) \rangle = \frac{1}{4\pi r^2 N}\left\langle \sum_{i=1}^N\sum_{j \neq i} \delta\left(|\mathbf{r}_i - \mathbf{r}_j| - r\right) \right\rangle Normalising by the bulk density \rho gives the radial distribution function: g(r) = \frac{1}{4\pi r^2\rho N} \left\langle \sum_{i=1}^N \sum_{j \neq i} \delta\left(|\mathbf{r}_i - \mathbf{r}_j| - r\right) \right\rangle = \frac{\langle \rho(r) \rangle}{\rho}
where \langle \rho(r) \rangle is the average density at distance r from a particle, and \rho is the bulk density.
Note
Hard spheres in 3D are not exactly solvable: we only have approximate theories (e.g. Percus-Yevick, below) and simulations. In 1D (hard rods) they are exactly solvable.
h\left(r_{12}\right)=c\left(r_{12}\right)+\rho \int c\left(r_{13}\right) h\left(r_{32}\right) d \mathbf{r}_3
where h(r) = g(r)-1. This is the Ornstein-Zernike integral equation between particles 1,2 and 3.
Both h(r) and c(r) are unknown in principle. One needs an additional condition to close the equation: these are physical closures leading to approximations.
Meaning of the Ornstein-Zernike relation, adapted from Santos, Springer(2016)
A common closure is the Percus-Yevick approximation.
c(r)=[1+h(r)]\left[1-e^{\beta V(r)}\right]
This closure interpolates between the hard-core exclusion (for V(r) \to \infty inside the core, g(r) = 0) and the ideal gas limit (for V(r) = 0, c(r) = 0, so for hard spheres c(r)=0 outside the core).
The result is (semi-)analytical. For hard spheres, it allows one to calculate the g(r) accurately in a wide range of packing fractions

The knowledge of the pair correlations also allows one to extract equation of states and significantly improve on the virial expansion, as the g(r) contains packing effects!
P=\rho k_B T-\frac{2 \pi \rho^2}{3} \int_0^{\infty} r^3 \frac{d V(r)}{d r} g(r) d r
Note
For hard spheres, V(r) jumps at contact, so write g(r)=y(r)\,e^{-\beta V(r)} with y(r) continuous. Since e^{-\beta V(r)} is a step at r=\sigma, \beta\frac{dV}{dr}\,g(r) = -y(r)\frac{d e^{-\beta V}}{dr} = -g(\sigma^+)\,\delta(r - \sigma)
Substituting into the pressure equation: P = \rho k_B T + \frac{2\pi\rho^2}{3} k_B T \sigma^3 g(\sigma^+)
Therefore, for hard spheres, the equation of state only requires knowledge of the contact value g(\sigma^+).
We will see this in a problem class.
The real-space correlations and relations have their reciprocal (Fourier space) counterparts.
The structure factor is defined as
S(k)=1+\rho \int[g(r)-1] e^{-i \mathbf{k} \cdot \mathbf{r}} d \mathbf{r}
Isotropicity in 3D simplifies the expression to
S(k)=1+4 \pi \rho \int_0^{\infty} r^2[g(r)-1] \frac{\sin (k r)}{k r} d r
Interestingly, reciprocal space simplifies integral equations such as Ornstein-Zernike
\tilde{h}(k)=\frac{\tilde{c}(k)}{1-\rho \tilde{c}(k)}
allowing one to read the direct correlation function directly from scattering data, as S(k)=1+\rho\tilde{h}(k).

Nothing prevents us from quantifying higher order correlations. In general these are non-trivial and controlled by the indirect part of the correlations.
Standard ways to identify n-particle correlations is to measure structural motifs.
Many body correlations in hard spheres, seminal work from Josh Robinson, PhD student in Bristol a few years ago, Robinson et al PRL (2019)
This is particularly important for dense systems (e.g. glasses, see future lecture).
The thermal motion of individual colloids is often well modeled via the Langevin equation
m \frac{d \vec{v}}{d t}=-\gamma \vec{v}+\vec{\eta}(t)
Coarse-graining over small volumes (and short times) gives us access to the local density \rho(\mathbf{r},t) which obeys a diffusion equation
\frac{\partial \rho(\mathbf{r}, t)}{\partial t}=D \nabla^2 \rho(\mathbf{r}, t)
The diffusivity is linked to the microscopic Langevin parameters via fluctuation-dissipation (Einstein’s relation)
D=\frac{k_B T}{\gamma}
(where the friction is the dissipation and the random force is the fluctuations).
It is possible to (re)-derive the diffusion equation solely from macroscopic requirements. We have a macroscopic density \rho(r,t) and a macroscopic flux \vec{J}(r,t)
\frac{\partial \rho(\mathbf{r}, t)}{\partial t}+\nabla \cdot \mathbf{J}(\mathbf{r}, t)=0 where the divergence \nabla \cdot \mathbf{J}(\mathbf{r}, t) represents the net outflow of particles from a given region due to the flux \mathbf{J}.
\mathbf{J}(\mathbf{r}, t)=-D \nabla \rho(\mathbf{r}, t)
It is immediate to combine the two to obtain the diffusion equation
\frac{\partial \rho(\mathbf{r}, t)}{\partial t}=D \nabla^2 \rho(\mathbf{r}, t)
The distribution \rho(\mathbf{r},t) encodes all the information about the motion of an ensemble.
Often, less is sufficient to characterise the diffusion. The second moment of the displacements (the mean squared displacement) provides this information. In d dimensions \left\langle \left| \mathbf{r}(t) - \mathbf{r}(t_0) \right|^2 \right\rangle = 2 d D t
Hence D can be extracted from linear fits to the MSD.
You have seen the Einstein relation for a Brownian particle with friction coefficient \gamma (Langevin dynamics): D=\frac{k_B T}{\gamma} (equivalently, in sedimentation equilibrium the drift flux n F/\gamma balances the Fickian flux -D\,\partial n/\partial x of the Boltzmann profile).
For a sphere, Stokes’ law \gamma=6 \pi \eta R yields simply
D=\frac{k_B T}{6 \pi \eta R}
Water, R=0.5\,\mum: D\approx0.5\,\mu\text{m}^2/\text{s}, so a colloid needs \tau_B=R^2/D\approx0.5 s to move its own radius (an atom: \sim10 ps). Colloidal liquids and crystals can be filmed under a microscope.
This is the Stokes-Einstein relation, a balance between thermal fluctuations and viscous dissipation:
\text { Fluctuations: } k_B T \quad \longrightarrow \quad \text { Observed motion: } D \quad \longrightarrow \quad \text { Dissipation: } 6 \pi \eta R .
Note
Consider hard spheres in a fluid.
At low volume fractions \phi they rarely collide and they perform overdamped (Brownian) dynamics. They will therefore diffuse as \operatorname{MSD} (t)= 6D_0 t
Things change when we increase the packing.

Stokes-Einstein breakdown in a theoretical model of glassy behaviour
| Topic | Key result |
|---|---|
| Colloidal scale | {\rm Pe}_g=\Delta m\, g R/k_BT\lesssim 1: Brownian motion beats sedimentation |
| Van der Waals | W_{vdW}(h)=-\frac{A_H}{6}f(h/R), attractive, \approx -A_HR/12D near contact |
| Double layer | W_{DR}(h)=B\frac{R}{\lambda_B}e^{-(h-2R)/\lambda_D} (gap h-2R), salt shortens \lambda_D |
| DLVO | W_{vdW}+W_{DR}: salt switches between stable and aggregating |
| Depletion (AO) | W_{AO}(r)=-k_BT\rho_p^r V_{\rm overlap}(r): entropic, -(1+\frac{3R}{2\delta})\phi_p^r k_BT at contact |
| Hard spheres | single control parameter \phi=\pi\sigma^3\rho/6; entropy only |
| Equation of state | dilute fluid Z_{\rm comp}=1+4\phi; crystal (cell model) Z_{\rm comp}=\left[1-(\phi/\phi_{cp})^{1/3}\right]^{-1} |
| Phase diagram | \phi_f=0.494, \phi_m=0.545, \phi_{cp}=0.74: the crystal has higher entropy |
| Structure | g(r) from imaging, S(k) from scattering; hard spheres Z_{\rm comp}=1+4\phi\, g(\sigma^+) |
| Diffusion | \langle\Delta r^2\rangle=2dDt; dense: D_0>D_s>D_L (cages) |
| Stokes-Einstein | D=\dfrac{k_BT}{6\pi\eta R}: fluctuation \leftrightarrow dissipation |
Full summary with links in the notes