Emission of N2O, N2, CH4, and CO2 from constructed wetlands for wastewater treatment and from riparian buffer zones

被引:179
作者
Teiter, S [1 ]
Mander, Ü [1 ]
机构
[1] Univ Tartu, Inst Geog, EE-51014 Tartu, Estonia
关键词
carbon dioxide; constructed wetland; dinitrogen; global warming potential; methane; nitrous oxide;
D O I
10.1016/j.ecoleng.2005.07.011
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
We measured nitrous oxide (N2O), dinitrogen (N-2) methane (CH4), and carbon dioxide (CO2) 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 N2O, N-2, CH4 and CO2 fluxes from the riparian gray alder stand varied from -0.4 to 58 mu g N2O-N m(-2) h(-1), 0.02-17.4 mg N-2-N m(-2) h(-1), 0.1-265 mu g CH4-C m(-2) h(-1) and 55-61 mg CO2-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 N2O-N emission from the microsites above the inflow pipes of the HSSF CWs was 6.4-31 mu g N2O-N m(-2) h(-1), whereas the outflow microsites emitted 2.4-8 mu g N2O-N m(-2) h(-1). In VSSF beds, the same value was 35.6-44.7 mu g N2O-N M-2 h(-1). The average CH4 emission from the inflow and outflow microsites in the HSSF CWs differed significantly, ranging from 640 to 9715 and from 30 to 770 mu g CH4-C m(-2) h(-1), respectively. The average CO2 emission was somewhat higher in VSSF beds (140-291 Mg CO2-C m(-2) h(-1)) and at the inflow microsites of HSSF beds (61-140 mg CO2-C m(-2) h(-1)). The global warming potential (GWP) from N2O and CH4 was comparatively high in both types of CWs (4.8 +/- 9.8 and 6.8 +/- 16.2 +/- CO2 eq ha(-1) a(-1) in the HSSF CW 6.5 +/- 13.0 and 5.3 +/- 24.7 t CO2 eq ha(-1) a(-1) in the hybrid CW, respectively). The GWP of the riparian alder forest from both N2O and CH4 was relatively low (0.4 +/- 1.0 and 0.1 +/- 0.30 t CO2 eq ha(-1) a(-1), respectively), whereas the CO2-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%. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:528 / 541
页数:14
相关论文
共 90 条
[11]   Denitrification and degassing in groundwater estimated from dissolved dinitrogen and argon [J].
Blicher-Mathiesen, G ;
McCarty, GW ;
Nielsen, LP .
JOURNAL OF HYDROLOGY, 1998, 208 (1-2) :16-24
[12]   Effects of wetting and drying on methane emissions from ephemeral floodplain wetlands in south-eastern Australia [J].
Boon, PI ;
Mitchell, A ;
Lee, K .
HYDROBIOLOGIA, 1997, 357 (1-3) :73-87
[13]   Are Phragmites-dominated wetlands a net source or net sink of greenhouse gases? [J].
Brix, H ;
Sorrell, BK ;
Lorenzen, B .
AQUATIC BOTANY, 2001, 69 (2-4) :313-324
[14]  
Brooks PD, 1997, OECOLOGIA, V110, P403, DOI [10.1007/PL00008814, 10.1007/s004420050175]
[15]   Reduction of forest floor respiration by fertilization on both carbon dioxide-enriched and reference 17-year-old loblolly pine stands [J].
Butnor, JR ;
Johnsen, KH ;
Oren, R ;
Katul, GG .
GLOBAL CHANGE BIOLOGY, 2003, 9 (06) :849-861
[16]  
BUTTERBACHBAHL K, 1997, P 11 WORLD FERT C CI, V2, P618
[17]   Global methane emission from wetlands and its sensitivity to climate change [J].
Cao, MK ;
Gregson, K ;
Marshall, S .
ATMOSPHERIC ENVIRONMENT, 1998, 32 (19) :3293-3299
[18]   Biotic controls on CO2 and CH4 exchange in wetlands -: a closed environment study [J].
Christensen, TR ;
Panikov, N ;
Mastepanov, M ;
Joabsson, A ;
Stewart, A ;
Öquist, M ;
Sommerkorn, M ;
Reynaud, S ;
Svensson, B .
BIOGEOCHEMISTRY, 2003, 64 (03) :337-354
[19]   NMR investigation of spin density wave repinning in (TMTSF)2PF6 [J].
Clark, WG ;
Hanson, ME ;
Wong, WH ;
Alavi, B .
JOURNAL DE PHYSIQUE IV, 1999, 9 (P10) :3-3
[20]  
COOPER AB, 1990, HYDROBIOLOGIA, V202, P13, DOI 10.1007/BF02208124