The theoretical possibility for evaluating the CO2 regime in the gaseo
us phase of chernozems on the basis of investigations into the soil ca
rbonate profile and secondary carbonates is discussed. A joint study o
f the carbon dioxide regime and the carbonate profile is thought to be
efficient, and a special method of performing such a study is propose
d. An attempt to test the method was made in a comparative study of no
nirrigated and irrigated chernozems. An approximate estimate of the co
ntribution from dissolution of carbonates to the additional CO2 efflux
from the soil surface at the beginning of irrigation is suggested.