Abstract
We measured nitrous oxide (N 2O), dinitrogen (N 2), methane (CH 4), and carbon dioxide (CO 2) fluxes in horizontal and vertical flow constructed wetlands (CW) and in a riparian alder stand in southern Estonia using the closed chamber method in the period from October 2001 to November 2003. The replicates’ average values of N 2O, N 2, CH 4 and CO 2 fluxes from the riparian gray alder stand varied from −0.4 to 58 μg N 2O-N m −2 h −1, 0.02–17.4 mg N 2-N m −2 h −1, 0.1–265 μg CH 4-C m −2 h −1 and 55–61 mg CO 2-C m −2 h −1, respectively. In horizontal subsurface flow (HSSF) beds of CWs, the average N 2 emission varied from 0.17 to 130 and from 0.33 to 119 mg N 2-N m −2 h −1 in the vertical subsurface flow (VSSF) beds. The average N 2O-N emission from the microsites above the inflow pipes of the HSSF CWs was 6.4–31 μg N 2O-N m −2 h −1, whereas the outflow microsites emitted 2.4–8 μg N 2O-N m −2 h −1. In VSSF beds, the same value was 35.6–44.7 μg N 2O-N m −2 h −1. The average CH 4 emission from the inflow and outflow microsites in the HSSF CWs differed significantly, ranging from 640 to 9715 and from 30 to 770 μg CH 4-C m −2 h −1, respectively. The average CO 2 emission was somewhat higher in VSSF beds (140–291 mg CO 2-C m −2 h −1) and at the inflow microsites of HSSF beds (61–140 mg CO 2-C m −2 h −1). The global warming potential (GWP) from N 2O and CH 4 was comparatively high in both types of CWs (4.8 ± 9.8 and 6.8 ± 16.2 t CO 2 eq ha −1 a −1 in the HSSF CW 6.5 ± 13.0 and 5.3 ± 24.7 t CO 2 eq ha −1 a −1 in the hybrid CW, respectively). The GWP of the riparian alder forest from both N 2O and CH 4 was relatively low (0.4 ± 1.0 and 0.1 ± 0.30 t CO 2 eq ha −1 a −1, respectively), whereas the CO 2-C flux was remarkable (3.5 ± 3.7 t ha −1 a −1). The global influence of CWs is not significant. Even if all global domestic wastewater were treated by wetlands, their share of the trace gas emission budget would be less than 1%.
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