The rate of CO
2 evolution
Y (g CO
2-
C/m
2/day) was studied
in situ of the several soils such as naked and farm land. The
Y of all soils was strongly controlled by soil temperature
T (°C) and increased exponentially with it. But the
Y of every soils showed considerable differences even when
T showed the same value. For example, when
T of all soils was almost the same of 22.5±0.5, there was about sixfold difference between
Y of 0.49 in naked land formed on Kanto-roam in Fuchu city and
Y of 2.83 in forest land adjacent to the naked land. The differences of the
Y were not attributable to the difference of soil water content, microbial number or nutritional minerals.
While, there were large differences in water soluble organic compound expressed in terms of carbon
C (mg
C/kg dry soil) from the smallest of 3 in naked land to the largest of 89 in farm land formed on alluvial land in Hachioji city. The
Y increased linearly with the increase of
C upto 50 in every soil, in which the regression equation obtained was
Y=0.022
C+0.51 at 18±2°C. When
C was over 50, the
Y was within the range between 1.5 and 1.7.
Namely, in spite of the difference of soil type, human impact and vegetation, it was concluded that the
Y could be determined by the two environmental factors in soil of
T and
C.
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