The carbon dioxide flux at the air/water interface in lakes was calculated
after the determination of H2CO3* (free CO2) and atmospheric CO2 using flow
injection analysis (FIA) coupled to a conductometric detector. The method
is based on the diffusion of CO2 through a hydrophobic membrane into a flow
of deionized water, generating a gradient of conductivity proportional to
the concentration of CO2 in the sample. Using one experimental set-up, the
speciation of the inorganic carbon (H2CO3* and dissolved inorganic carbon)
was accomplished by simply adjusting the sample pH. The determination of CO
2 in the atmosphere was carried out by direct injection of the gaseous samp
les. The FIA apparatus was taken into the field and CO2 fluxes were evaluat
ed in several Brazilian lakes. In these lakes, representing different eutro
phic stages, the CO2 flux varied from -242 (invasive) up to 3227 (evasive)
mu mol CO2 m(-2) h(-1).