Natural variability of carbon dioxide and net epilimnetic production in the surface waters of boreal lakes of different sizes

Citation
Ca. Kelly et al., Natural variability of carbon dioxide and net epilimnetic production in the surface waters of boreal lakes of different sizes, LIMN OCEAN, 46(5), 2001, pp. 1054-1064
Citations number
36
Categorie Soggetti
Aquatic Sciences
Journal title
LIMNOLOGY AND OCEANOGRAPHY
ISSN journal
00243590 → ACNP
Volume
46
Issue
5
Year of publication
2001
Pages
1054 - 1064
Database
ISI
SICI code
0024-3590(200107)46:5<1054:NVOCDA>2.0.ZU;2-U
Abstract
The variability of surface water carbon dioxide concentration, or partial p ressure (pCO(2)) was studied in 11 lakes of greatly varying size (2.4 ha up to 8 million ha) in Northwest Ontario, Canada. Six of these lakes were cho sen to be as similar as possible in all respects except surface area (the N orthwest Ontario Lake Size Series [NOLSS], which range from 88 to 35,000 ha ). Spatial and temporal variability of pCO(2) within a single lake was no g reater in the larger lakes than in the smaller lakes. Interannual variabili ty was significant and synchronous, which indicates that weather patterns w ere important and affected the different lakes within the region in a simil ar manner. However, annual pCO(2) averages were not related to annual diffe rences in planktonic photosynthetic activity, measured by (CO2)-C-14 fixati on. In the six NOLSS lakes, there was not a significant relationship of ave rage pCO(2) with lake size. For all 11 lakes, however, there was a signific ant negative correlation of pCO(2) with lake size, which was likely due to several characteristics of the very small and very large lakes that covarie d with size. The larger lakes were deeper and had longer water residence ti mes and lower DOC, which suggests lower CO2 production from allochthonous o rganic carbon inputs. Also, the ratio of epilimnetic sediment area/epilimne tic volume (A(e)V(e)) was smaller in the larger lakes, which likely resulte d in lower rates of recycling of fixed carbon to CO2 during summer stratifi cation.