An investigation of simulations of one dimensional distributions of CO
2concentrations in soils was made. For the simulation, the coefficients of CO
2 diffusion in a soil
D (
x) were required. The relation between the diffusion coefficient (
D) and air permeability (
K) in this experiment, was found the following equations.
D=0.093 cm
2/sec at
K≥1.2 cm/sec
D=0.0845
K0.432cm
2/sec at
K≤1.2cm/sec
As it was very difficult to determine the
D (
x) of a soil, the
D (
x) was estimated from the equations above after determining the air permeability
K (
x) . Then, we made the assumption that the amount of CO
2 generated in a soil is expressed by the following equation
Pco
2 (
t) =
Ae-B (logt/Tm) 2+
CconstC (
l)
pv was the CO
2 concentration at the bottom of a soil, and was calculated by the
Pco
2 change with time.
C (
l)
pc also was the CO
2 concentration at the same place, and was calculated by assuming that the amount of
PCO
2 when the CO
2 concentration was determined was constant throughout the experiment.
Comparing
C (
l)
pv with
C (
l)
pc, we found that
C (
l)
pv was about 0.9-1.6 times as great.
Therefore, distribution of the CO
2 concentration could not be expressed as
C (
x) so far as the parameters in the equation of
PCO
2 are concerned. When the CO
2 concentration at the bottom of a soil was taken as 1 (=
RC (
l) ), and all the CO
2 concentrations in a soil were taken as
RC(
x) =
C (
x) /
C (
l), distributions of the CO
2 concentrations in soils were found to be regular regardless of the parameters in the equations of
Pco
2. Therefore, to express the distributions of the CO
2 concentrations, we used
RC (
x) which denotes the relative concentrations of CO
2.
The distributions determined and those simulated by the expression above agreed very wll. Thus, the one dimensional distributions in a soil could be simulated.
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