Environmental Engineering Reference
In-Depth Information
Table 5.1 Half-lifes of selected radionuclides
Radionuclide
Half-life
Radionuclide
Half-life
10 9 years
U-238
4.5
H-3
12.35 years
U-235
32,500 years
Ra-228
5.8 years
Ra-226
1,600 years
Th-228
1.91 years
Am-241
432.2 years
Gd-153
242 days
Pu-238
87.74 years
Po-210
138 days
Cs-137
30 years
Sr-89
50.5 days
Pb-210
22.3 years
Th-234
24.1 days
From mathematical point of view, the major difference between radioactive
decay and other forms of first order losses lies in the decay constant. The half-life
of radionuclides is constant under all conditions known. The rate of exponential
decay of a nuclide is not influenced by any environmental condition, neither by
temperature, nor by pressure, nor by the biogeochemical surrounding. Table 5.1
lists some radionuclides and their half-lifes. The simulation of a chain of
radionuclides is described in Chap. 18.2.
In contrast, chemical and biochemical rates are strongly affected by environ-
mental variables. In fact, the decay law can often be understood as a most simplified
rule, in which the interaction of several complex processes are gathered and where
l
is a lumped parameter. Clearly, in a changed environment the parameter is differ-
ent. More complex degradation rules, using the Michaelis-Menten or Monod
kinetics, are treated below (see Chap. 7).
5.2
1D Steady State Solution
As mentioned above, the differential equation for the steady state is obtained by
setting the time derivatives in the transport ( 5.2 ) to zero. The right hand side of the
1D transport equation has thus been set to zero:
@x D @ c
@
@x v @c
@x l c ¼
0
(5.7)
This is an ordinary differential equation for the independent variable x .With
MATLAB
ordinary differential equations can be solved numerically (see Chap. 9).
Here, an analytical solution, which provides the solution in an explicit formula, is an
alternative if the coefficients are constants, i.e. independent of x and t .Inorderto
solve differential ( 5.7 ) analytically, it is appropriate to note it in a different form:
®
c ¼
@
@x m 1
@
@x m 2
0
(5.8)
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