Determination of 222 Rn Diffusion Coefficient in Japanese Soils
Determination of 222 Rn Diffusion Coefficient in Japanese Soils
Determination of 222 Rn Diffusion Coefficient in Japanese Soils
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P-1b-48<br />
Compartment 2<br />
V2 C2<br />
Sample soil<br />
Co(z) Po<br />
Compartment 1<br />
V1 C1<br />
<strong>Rn</strong> source<br />
z<br />
z= Ho<br />
z=0<br />
Figure 1 The schematic cross section <strong>of</strong> diffusion chamber.<br />
The time dependent equation describ<strong>in</strong>g the concentration, C 0 , is given by Fick’s Law:<br />
dC<br />
dt<br />
0<br />
D<br />
0<br />
d<br />
2<br />
0<br />
2<br />
dz<br />
C<br />
+ P − λC<br />
= (1)<br />
where λ =the decay constant for <strong>222</strong> <strong>Rn</strong>.<br />
dC<br />
dt<br />
0 =<br />
0<br />
In steady state 0 and Eq.1 transforms <strong>in</strong>to:<br />
d<br />
2<br />
0<br />
2<br />
dz<br />
C<br />
C<br />
P<br />
0<br />
0<br />
− λ 0 = −<br />
(2)<br />
D0<br />
D0<br />
The boundary conditions at equilibrium are:<br />
C 0 (z=0)=C 1 and C 0 (z=H 0 )=C 2 (3)<br />
Eq (2) becomes<br />
d<br />
2<br />
0<br />
2<br />
dz<br />
with<br />
C<br />
C<br />
P<br />
0 0<br />
− = −<br />
(4)<br />
2<br />
l0<br />
D0<br />
2 D0<br />
l<br />
0 = ,<br />
0<br />
λ<br />
l =diffusion length.<br />
The solution <strong>of</strong> Eq.4 is given as:<br />
⎛ z ⎞ ⎛ z ⎞ P<br />
C0 () z As<strong>in</strong>h<br />
⎜ B cosh +<br />
l<br />
⎟<br />
⎜<br />
0<br />
l<br />
⎟<br />
⎝ ⎠ ⎝ 0 ⎠ λ<br />
0<br />
= +<br />
(5)<br />
From the boundary conditions <strong>in</strong> Eq.3 it follows that:<br />
C<br />
=<br />
C cosh β − P0 (1<br />
s<strong>in</strong>h β<br />
2 − 1<br />
−<br />
cosh β ) / λ<br />
A (6a)<br />
B<br />
C<br />
1<br />
P0<br />
−<br />
λ<br />
= with<br />
H<br />
=<br />
l<br />
0<br />
β (6b)<br />
0<br />
2