Abstract
The relationship between CO(2) flow from soil and soil CO(2) concentration was investigated at 72 permanent sampling points at two forested post-mining sites in the northwest of the Czechia. Based on the entire data set (72 points sampled monthly during the growing season), CO(2) flow from the soil was positively correlated with soil CO(2) concentration. CO(2) concentration in deeper soil layers was positively correlated with root biomass and negatively correlated with soil microbial respiration. In individual sampling points relationship between CO(2) flow and soil CO(2) concentration varied from being significantly positive (30% of points) to significantly negative (7%) but mostly being non-significant (63%). The positive correlation occurred at points with high root biomass in deeper soil layers, while the negative correlation occurred at points with high soil microbial respiration per cm(3) of soil. Laboratory experiments showed that the CO(2) produced by microbial respiration can reduce microbial respiration but that CO(2) produced by root respiration did not reduce root respiration. The results indicate that when soil ventilation is poor, microbial respiration can sufficiently increase soil CO(2) concentration so as to reduce microbial respiration, which greatly increases the variability in the relationship between CO(2) flow from soil and soil CO(2) concentration.