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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

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