2017
DOI: 10.1016/j.ecoleng.2016.10.027
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Convective transport of dissolved gases determines the fate of the greenhouse gases produced in reactive drainage filters

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Cited by 15 publications
(12 citation statements)
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“…Retention of organic N accounted for 4 to 7% of the annual net TN removal. Greenhouse gas emissions in the CWs (Bruun et al, 2017) demonstrated that the amount of N 2 O‐N dissolved in the outflow ranged from 28 to 101 g N 2 O‐N m −2 yr −1 , supporting the finding that the major removal pathway of NO 3 was denitrification, with N 2 O production accounting for 2 to 5.5% of the N removal by the denitrification process.…”
Section: Discussionsupporting
confidence: 57%
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“…Retention of organic N accounted for 4 to 7% of the annual net TN removal. Greenhouse gas emissions in the CWs (Bruun et al, 2017) demonstrated that the amount of N 2 O‐N dissolved in the outflow ranged from 28 to 101 g N 2 O‐N m −2 yr −1 , supporting the finding that the major removal pathway of NO 3 was denitrification, with N 2 O production accounting for 2 to 5.5% of the N removal by the denitrification process.…”
Section: Discussionsupporting
confidence: 57%
“…The volume (m 3 ) of the distribution layer ( V 1 ) and the woodchips–seashell filter media ( V 2 ) was obtained from the measured depth and cross‐sectional area of each layer in the filter beds. The water‐filled porosity (m 3 m −3 ) for the distribution layer (θ 1 ) and the woodchips–seashell filter media (θ 1 ) was obtained for each material from the dry bulk density ρ b (kg m −3 ), the density of water (ρ w ), and the gravimetrical water content w dm (kg kg −1 ) measured from laboratory columns by Bruun et al (2017) according to the method described by Kjaergaard et al (2012). Dry bulk density (ρ b ) in the columns was determined from sample volume and sample dry weight after oven drying at 105°C (Table 1): θ=(normalρnormalb/normalρnormalw)wdm …”
Section: Methodsmentioning
confidence: 99%
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“…CH4 emission fluxes were also comparable to those measured in wetlands (4-49 mg/(m 2 ꞏh)) (Whalen, 2005;Audet et al, 2013), constructed wetlands (1-47 mg/(m 2 ꞏh)) (Søvik et al, 2006) and undisturbed natural soil (1-20 mg/(m 2 ꞏh)) (Yang et al, 2013), and much lower than those measured in landfills (96 g/(m 2 ꞏh)) (Bruun et al, 2017 and references therein). Finally, N2O flux values measured for the PRB fell in the lower end of values reported in literature in riparian soils (0.02-31 mg/(m 2 ꞏh)) (Audet et al, 2013;Audet et al, 2014;Hinshaw and Dahlgren, 2016;Jurado et al, 2017 and references therein), European agricultural and forested ecosystems (0.4-137 mg/(m 2 ꞏh)) (Machfert et al, 2002) and constructed wetlands (<0.01-58 mg/(m 2 ꞏh)) (Søvik et al, 2006;Bruun et al, 2017). These values of N2O have been reported to not represent a significant contribution to the atmosphere compared to the direct emissions from agricultural fields (Hinshaw and Dahlgren, 2016;Jurado et al, 2017).…”
Section: Gases Analysismentioning
confidence: 45%