Biomedical Engineering Reference
In-Depth Information
Figure 10.1  Distribution of charges around a spherical particle of radius a . The gray halo represents
the cloud of counterions.
This classical calculation starts by writing the Poisson equation that relates the
potential y to charge density r :
ρ
2
Ñ
ψ
= -
(10.1)
ε ε
0 r
where e 0 is the vacuum permittivity (» 8.85·10 -12 C 2 J -1 m -1 ) and e r the relative per-
mitivity (» 80 for water).
At equilibrium, r is given by summing the number of charges in the solution.
The number n i of ions of each species is given by a Boltzmann distribution:
n
=
n
0 exp(
-
z e
ψ
/
k T
)
(10.2)
i
i
i
B
z i is the valency of the ions, e is the elementary charge (1 eV = 1.6·10 -19 C), k B the
Boltzmann constant (~ 1.38·10 -23 J.K -1 ) and T the temperature. n i0 is the number of
these ions far from the surface. The charge density is then given by:
å
ρ
=
n z e
=
n
0 (
-
ze
×
exp(
-
ze
ψ
/
k T
)
+
ze
×
exp(
ze
ψ
/
k T
))
(10.3)
i
i
B
B
i
in the case of symmetric electrolytes.
The Gouy-Chapman model combines (10.1) and (10.3), the boundary con-
ditions being given by the global electro-neutrality condition and by the surface
charge.
In a plane geometry, this equation can be solved analytically but the case
ey<<k B T is instructive (Debye-Hückel approximation). The linearization of (10.3)
then leads to the classical expression:
ψ ψ
=
0 exp(
×
- ×
κ
x
(10.4)
 
Search WWH ::




Custom Search