
Most lakes are super-saturated in CO2 and emit greenhouse gases to the atmosphere.
The in-situ transformation of dissolved organic carbon (DOC) imported from the terrestrial landscape to dissolved inorganic carbon (DIC) constitutes a major source of CO2 for aquatic ecosystems.
Regional specificities regarding the origin and composition of DOC generate contrasting relationships between DOC and the partial pressure of CO2 (pCO2), the main determinant of lakes greenhouse gases emission. This results that the observed pCO2 may vary by more than an order of magnitude for a given concentration of DOC.
The overall objective of my thesis is to refine our understanding of the role of DOC as a substrate for the production of CO2 in boreal lakes. More specifically, the main approach is to examine the links between catchments regional characteristics, DOC composition and origin and its biological and photo-chemical reactivity.
| < Prev | Next > |
|---|