Summer fluxes of atmospheric greenhouse gases N2O, CH4 and CO2 from mangrove soil in South China

• DOI: 10.1016/j.scitotenv.2010.03.007
• Publication Date: 2010-04-12T07:02:55Z
• Authors: G.C. Chen; N.F.Y. Tam; Y. Ye
• Keywords: Greenhouse Effect; China; Geologic Sediments; Nitrogen Dioxide; 551; 01 natural sciences; CARBON-DIOXIDE; Soil; HEAVY-METALS; METHANE EMISSION; Soil Pollutants; ESTUARY; Seawater; INDIAN MANGROVE; NE COAST; 0105 earth and related environmental sciences; Carbon Dioxide; 15. Life on land; 13. Climate action; SPATIAL-DISTRIBUTION; HONG-KONG; Avicennia; Seasons; NITROUS-OXIDE FLUX; Methane; SEDIMENTS; Environmental Monitoring

The atmospheric fluxes of N(2)O, CH(4) and CO(2) from the soil in four mangrove swamps in Shenzhen and Hong Kong, South China were investigated in the summer of 2008. The fluxes ranged from 0.14 to 23.83 micromol m(-2)h(-1), 11.9 to 5168.6 micromol m(-2)h(-1) and 0.69 to 20.56 mmol m(-2)h(-1) for N(2)O, CH(4) and CO(2), respectively. Futian mangrove swamp in Shenzhen had the highest greenhouse gas fluxes, followed by Mai Po mangrove in Hong Kong. Sha Kong Tsuen and Yung Shue O mangroves in Hong Kong had similar, low fluxes. The differences in both N(2)O and CH(4) fluxes among different tidal positions, the landward, seaward and bare mudflat, in each swamp were insignificant. The N(2)O and CO(2) fluxes were positively correlated with the soil organic carbon, total nitrogen, total phosphate, total iron and NH(4)(+)-N contents, as well as the soil porosity. However, only soil NH(4)(+)-N concentration had significant effects on CH(4) fluxes.