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Our study investigated the concentration of dissolved carbon at the point when water leaves the pedosphere and whether this amount represents a significant proportion of terrestrial carbon cycling. The investigations were carried out in a temperate forest catchment (Black Forest, Germany) over a period of 1 year. The annual export of dissolved C compounds (14.4 g C m(-2) year(-1)) was dominated by CO(2) (9.7 vs. 4.7 g C m(-2) year(-1) DOC). Even though the direct CO(2) degassing at the spring...Our study investigated the concentration of dissolved carbon at the point when water leaves the pedosphere and whether this amount represents a significant proportion of terrestrial carbon cycling. The investigations were carried out in a temperate forest catchment (Black Forest, Germany) over a period of 1 year. The annual export of dissolved C compounds (14.4 g C m(-2) year(-1)) was dominated by CO(2) (9.7 vs. 4.7 g C m(-2) year(-1) DOC). Even though the direct CO(2) degassing at the spring was inferior (0.4 kg C year(-1)), considerably lower CO(2) concentrations were measured 17 m downstream of the spring. This shows that a large proportion of dissolved CO(2) (93%) originating from the pedosphere is not captured anymore within a short distance from the spring. The measured lateral C-transport was in the same order of magnitude as reported for the net ecosystem exchange (NEE) observed for German spruce forests (-4 to -55 g C m(- 2) year(-1)). Therefore, the results clearly demonstrated that the lateral transport of dissolved carbon can be a significant part of terrestrial carbon budgets and for this study site CO(2) was dominating this índirect' pathway. However, for generalisation, it is important to extend this investigation to other landscapes and climatic zones.» weiterlesen» einklappen

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