Biomedical Engineering Reference
In-Depth Information
always exists an orbital effect regardless of particle distribution in
ensembles.
Considering the helical motion given by Eq. (4.15a-b) the
collision period for the ion to transverse the mean free path is
modified, increasing a with an increasing B field, compared with
the unperturbed path. This is obtained by considering the radial
displacement in the XY plane and using Eq. (4.15a-b) to solve for
the modified time t m .
c t col 1
1
ω c
π ar cos( 1
t m =
2 ω
(4.17)
Expanding the perturbed collision period as a Taylor series
where ω c t col << 1, we get
t m = t col + ω
c t col
c t col
c t col
3 ω
5 ω
24 +
640 +
7168 + ...
(4.18)
Analogous to free-space cyclotron motion (Chen, 1974), and
similar to the findings of Kinouchi et al. (1988), the
ρ
offsets of the
B field are thus found to retard diffusion in the transverse plane.
This effect modifies the Nernst-Planck equation relating ionic flux
to Fick'sdiffusion andE field mobility(Plonsey andBarr, 1988).
j T =−
μ Ca E (4.19)
since in the hard-sphere model Fick's constant is dependent upon
the mean ionic total velocity, v th , and the mean free path, d :D =
v th d /3 (Reif, 1965; Plonsey and Barr, 1988). The total particle flux,
j D ,duetobothFick'sdiffusion, j F ,andtheretardationeffectoftheB
field, j B , is written as j D = j F + j B where
j B = D μ
D
C
+
C
Ca B 2
24 C
B × n
(4.20)
where D is Fick's constant, C is the concentration gradient in
Mm 1 and the orbital effect upon ions in the ˆ
θ direction is assumed
negligibleatmacroscopic levels.
The retardation effect of the B field upon the diffusion rate may
be estimated. For example, if B is 60 μ T, a typical LGF strength, an
estimate of relative difference in D ( μ
2
Ca B 2
24 )iscomputedas6.9 ×
a Infact,ifthecollisionperiodswereallconstant,andsynchronouswiththecyclotron
frequency, there would be no transverse diffusion, because the ion would orbit one
complete transverse circularpath.
 
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