Paper summarize and discuss measurements from Lekinka Cave, where interactions at rock-water (dissolution) and water-air (flux of CO2) interfaces were investigated. We found out important feed-back mechanism between channel morphology and rate of CO2 outgassing, which influences present-day genesis of Lekinka Cave. To carry out all research topics, limestone tablets, physico-chemical analyses of water, measurements of CO2 fluxes between water and air, and modelling with PHREEQC were used as appropriate methodology.
COBISS.SI-ID: 35231533