Summer depth distribution profiles of dissolved CO2 and O2 in shallow temperate lakes reveal trophic state and lake type specific differences
| Autor: | Peeter Nõges, Pille Meinson, Tiina Nõges, Alo Laas, Fabien Cremona, Eva-Ingrid Rõõm |
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| Rok vydání: | 2016 |
| Předmět: |
0106 biological sciences
Hydrology Environmental Engineering 010504 meteorology & atmospheric sciences Mixed layer 010604 marine biology & hydrobiology Alkalinity Carbon sink Atmospheric sciences 01 natural sciences Pollution Carbon cycle Atmosphere chemistry.chemical_compound chemistry Carbon dioxide Environmental Chemistry Environmental science Surface layer Waste Management and Disposal 0105 earth and related environmental sciences Trophic level |
| Zdroj: | Science of The Total Environment. :63-75 |
| ISSN: | 0048-9697 |
| DOI: | 10.1016/j.scitotenv.2016.05.038 |
| Popis: | Knowledge about dissolved oxygen (DO) and carbon dioxide (CO2) distribution in lakes has increased considerably over the last decades. However, studies about high resolution dynamics of dissolved CO2 in different types of lakes over daily or weekly time scales are still very scarce. We measured summertime vertical DO and CO2 profiles at sub-hourly intervals during one week in eight Estonian lakes representing different lake types according to European Water Framework Directive. The lakes showed considerable differences in thermal stratification and vertical distribution of dissolved oxygen and CO2 as well as different diurnal dynamics over the measurement period. We observed a continuous CO2 supersaturation in the upper mixed layer of the alkalitrophic (calcareous groundwater-fed) lake and the dark soft-water lake showing them as CO2 emitting "chimneys" although with different underlying mechanisms. In three lake types strong undersaturation with CO2 occurred in the surface layer characterising them as CO2 sinks for the measurement period while in another three types the surface layer CO2 was mostly in equilibrium with the atmosphere. Factor analysis showed that DO% in the surface layer and the strength of its relationship with CO2% were positively related to alkalinity and negatively to trophic state and DOC gradients, whereas deeper lakes were characterised by higher surface concentration but smaller spatial and temporal variability of CO2. Multiple regression analysis revealed lake area, maximum depth and the light attenuation coefficient as variables affecting the largest number of gas regime indicators. We conclude that the trophic status of lakes in combination with type specific features such as morphometry, alkalinity and colour (DOC) determines the distribution and dynamics of dissolved CO2 and DO, which therefore may indicate functional differences in carbon cycling among lakes. |
| Databáze: | OpenAIRE |
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