1experimental evidence of the presence of electrical charge of particles suspended in a polar liquid medium such as water
when an electric field is applied to a suspension, in most cases there will be a net displacement of the particles in the direction parallel to the field
2the reason for ion accumulation on the liquid phase of an interface
the presence of charge of any sign on the particle surface requires, for an electrically neutral system, a charge of opposite sign and the same magnitude on the liquid phase side
3the reason for asymptotic decay of electrostatic potential from the surface toward the bulk solution value
thermal agitation in the liquid phase distributes ions (which would otherwise attach to the particle surface) toward the bulk of the solution
4the equilibrium condition for any chemical species across phase boundaries
the constancy of the chemical potential ($μ^α = μ^β = …$)
5the result of charged species (ion) presence in the interfacial region
an additional electrical work is involved in the transference of matter between phases due to differing electrostatic potential of each phase
6electrochemical potential
$μ^α := μ^α_0 + z_i F ψ^α$, where z is the charge of ion i, F is the Faraday constant, $ψ^α$ is the electrostatic potential of phase α
7Poisson equation (1D)
$\nabla^2ψ=\frac{d^2ψ}{dx^2}=–\frac{ρ_q}{ε}$, where ψ is the electrostatic potential at any point in space with fixed charge density $ρ_q$ (i.e., electrical charge per unit volume) and ε is the dielectric coefficient (or constant) of the medium
8conceptualization of the Poisson equation considering mobile ions (i.e., $ρ_q$ varies spatially)
in the absence of external forces, the motion of the charges in solution is random so that we can consider an average distribution; when the system is in thermal equilibrium (or close to it) the ions must follow the Boltzmann distribution
9Boltzmann distribution of ion molar concentration
$c_i(r) = c^\infin e^\frac{–z_i e ψ(r)}{kT}$, where c(r) is the molar concentration of ion i at the point r in space, ψ(r) is the potential at the same point, $c^\infin$ is the concentration of the same ion in the solution bulk, z is the charge of that ion, e is the elementary charge, (exp e is the Euler's number), k is the Boltzmann constant and T the absolute temperature
10charge density at any point in space
$ρ_q(r)=\Sigma z_i F c_i(r)$
11the Poisson-Boltzmann (PB) equation
$\nabla^2 \psi(r) = -\frac{F}{ε} \Sigma z_i c^\infin_i e^\frac{–z_i e ψ_i(r)}{kT} = -\frac{F}{ε} \Sigma z_i c^\infin_i e^\frac{–z_i F ψ_i(r)}{RT}$, where the rightmost expression is fully written in molar units, R being the molar gas constant; the summation extends over all the ionic species present in the solution
12assumptions of the PB equation applied to a solution containing ions
the solution is considered to be a continuous medium of constant ε, and the ions are considered point charges
13linearization of the PB equation
$e^{-\frac{z_i F \psi}{RT}}≈1-\frac{z_i F \psi}{RT}$
14validity of linearized PB equation
valid for $\frac{z_i F \psi}{RT}<1$ or ψ < 25 mV
15PB solution with Debye–Hückel theory
$\psi (r)=\frac{ze}{4 \pi εr} \frac{e^{κ(r_0-r)}}{1+κr_0}$
16diffuse layer (ion atmosphere)
the region where potential and concentration values differ from those at the bulk phase but decay toward it asymptotically (when around a particle or single ion, respectively)
17Debye length OR diffuse layer thickness
$κ^{-1}$ where $κ=\sqrt{\frac{2F^2I}{εRT}}$
18ionic strength
$I=\frac{1}{2} \Sigma z^2_i c^\infin_i$, an important property of electrolyte solutions
19importance of ionic strength
determines (near the central ion): κ, concentration profiles
20the reason for invalidity of the linearized PB equation for colloidal systems
in the case of spherical particles, where the Debye–Hückle theory can be in principle applied, the radius is greater, which would make the surface potential lower, but the total charge is several times that of a single ion, leading to a relatively high surface potential
21Gouy–Chapman (GC) theory
a treatment of the PB equation in which the diffuse layer is in contact with a plane, infinite surface having a nonzero surface charge density $\sigma_s$
22double layer
the two oppositely charged regions at both sides of the interface, which can also be regarded as a capacitor
23similarity of the double layer to a capacitor
there are charges of opposite sign and equal magnitude at both sides of the interface
24the reason for invalidity of the GC model
in the GC model, there is no separation in the double layer, resulting in the capacitance (per unit area) going to infinity (consider $C=\frac{ε}{d}$ [per unit area])
25differential interfacial capacitance (interfacial capacitance)
$C=\left( \frac{\partial \sigma_s}{\partial \Delta \psi} \right)_{T,P,\mu_i} =\left( \frac{\partial \sigma_s}{\partial \psi_0} \right)_{T,P,\mu_i}$, where $\Delta \psi$ is the potential difference across the interface; in the right-hand side, it has been considered that $\psi=0$ in the solution bulk
26Stern plane (“2” plane)
the distance of closest approach to the surface for an ion, located at $x_2$ so that the properties of the diffuse layer may be found using the framework of the GC theory by replacing $\psi_0$ with $\psi_2$ and $x$ with $x-x_2$
27inner layer
• the space between the Stern plane (“2” plane) and the surface
• filled with solvent
• behaves as a dielectric
28Stern modification of GC theory (GCS)
from an electrical point of view, the model interprets the double layer as two capacitors in series, i.e., $\frac{1}{C}=\frac{1}{C_i}+\frac {1}{C_d}$, where $C_i$ is the inner layer or Stern capacitance, and $C_d$ is the diffuse layer capacitance given by the GC theory
29significance of minimum capacitance in the Gouy–Chapman–Stern theory
the minimum capacitance is identified as the point where the surface charge becomes null; here, the diffuse layer capacitance is determining the total surface capacitance (because in a series connection, the lower capacitance dominates the result), and as $C_d$ shows a minimum when both $\psi_2$ and $\sigma_d$ vanish, the potential (measured against a reference) of the electrode at this point should correspond to zero surface charge
30experimental determination of point of zero charge
- determined by the potential on conducting electrodes under external control
- on nonconducting and/or isolated surfaces, it is determined by the medium conditions, usually the pH
31Grahame modification of the Gouy–Chapman–Stern theory (GCSG)
the Gouy–Chapman–Stern theory predicts well the interfacial capacitance of the interface between mercury electrodes and some electrolytes such as NaF or NaClO4, but fails for others such as KCl or KI; this is due to the fact that some ions, especially polarizable anions such as Br- and I-, can reach the surface closer than the Stern plane; thus *two* planes of closest approach are defined
32inner Helmholtz plane (IHP)
the plane of closest approach located at $x_1$, the distance between the surface and the center of ions with which it is in direct contact, and with potential $\psi_1$
33outer Helmholtz plane (OHP)
the plane of closest approach located at $x_2$, the distance between the surface and the center of ions that are separated by a layer of water molecules, and with potential $\psi_2$
34context of these electrified interface descriptions
these descriptions are based on a metallic electrode in laboratory conditions under potential control, a situation that is not, in principle, representative of what can be found in a complex natural system as a soil; these results are presented because liquid mercury is a surface as devoid of structure as possible so that the contributions to the charge from the solution side were focused upon; nevertheless, the diffuse layer, OHP and IHP are all present in the interaction between colloidal particles and solution
35ideal gas constant
$R=k_BN_A=1.381(10^{-23}) \text{ J/K}*6.022(10^{23}) \text{ entities/mol}=8.314 \text{ J/(K-mol)}$
36Faraday constant
$F=\frac{e}{n}=(e)(N_A)=1.602(10^{-19}) \text{ C}*6.022(10^{23}) \text{ entities/mol}=96.5(10^3) \text{ C/mol}$