Concentration dependence of CO2 evolution from soil was studied under field and laboratory conditions. Under field conditions, when the CO2 concentration was measured with an infrared gas analyzer (IRGA) in a small and column-shaped chamber placed on the ground, the relationship among the CO2 concentration c (m3 m-3), time t (h), height of the chamber h, a constant rate of CO2 evolution from the soil upsilon (m3 m-2 h-1), and an appropriate constant k, was expressed by the following equation, dc/dt = upsilon/h-k(c-a) (c = a at t = 0). Although most of the data of measured CO2 evolution fitted to this equation, the applicability of the equation was limited to the data to which a linear equation could not be fitted, because the estimated value of v had a larger error than that estimated by linear regression analysis, as observed by computer simulation. The concentration dependence shown above and some other variations were analyzed based on a sorption/diffusion model, i.e. they were associated with CO2-sorption by the soil and modified by the conditions of CO2 diffusion in the soil.