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Spatiotemporal Variations Of Nitrous Oxide (N2O) Concentrations And Flux In17Reservoirs And Their Input Rivers Of Guangdong Province

Posted on:2013-05-19Degree:MasterType:Thesis
Country:ChinaCandidate:X M ZhangFull Text:PDF
GTID:2230330362965543Subject:Environmental Science
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Environmental problems were caused by atmospheric N2O concentration risingthrough global temperature increasing and ozone destruction. Clearing atmosphericN2O emission sources, their N2O distribution and release characteristics issignificance to control atmospheric warming. The reservoirs are widely distributed inlarger quantities, but the reservoir whether N2O emission source remaining incontroversy.In order to decide whether the reservoirs and their input rivers can be consideredas the N2O emissions source, and understanding the distribution characteristics ofN2O of reservoirs and their input rivers, this study chose the six River Basin ofGuangdong Province (coastal western Guangdong, the Xijiang River, the North Riverbasin, the East River basin,17large and medium-sized reservoirs in the Pearl RiverDelta and eastern Guangdong coastal) as the research objectives, the N2O distributionand release characteristics, source and sink and their influencing factors wereresearched. The major findings of this paper were as follows:The concentrations and water-atmosphere fluxes of dissolved N2O in17reservoirs and rivers of Guangdong Province were investigated during the wet seasonand the dry season,2011. N2O concentration in the surface waters were measured bypurge and trap-gas chromatography. The results demonstrated that reservoirs and theirinput rivers kept lower N2O concentration in the wet season than the dry season, withsignificant seasonal variations (P<0.01). Seeing from Spatial variation, changingtrends of dissolved N2O concentrations was Pearl Delta area> Coastal area in westGuangdong> Coastal area in east Guangdong> Beijiang watershed> Dongjiangwatershed. In flooded season, N2O concentration in the surface waters were lowerthan in the bottom waters(P<0.01). At the same time, vertical distribution of reservoirN2O dissolved concentrations were significantly different both in the dry season andin the wet season. In addition to Changhu and Songmushan Reservoirs, the N2Odissolved concentrations of other reservoirs were all lower in the surface water than in the bottom water (P<0.01), had layered phenomenon. The N2O dissolvedconcentrations of the surface water and bottom water in reservoirs had no significantrelationships (P>0.01) in dry season. Deposit concentration compared with otherwaters, N2O dissolved concentrations of reservoirs and their input rivers were in themedium level.The saturations of reservoirs and their input rivers were calculated through N2Odissolved concentration. The results demonstrated that reservoirs and their input riverskept lower N2O saturations in flooded season than dry season, with significantseasonal variations (P<0.01). Seeing from Spatial variation, changing trends of N2Osaturations was Pearl Delta area> Coastal area in west Guangdong> Coastal area ineast Guangdong> Beijiang watershed> Dongjiang watershed. In wet season, N2Osaturations in the surface waters were lower than in the bottom waters (P<0.01). Atthe same time, vertical distribution of reservoir N2O saturations concentrations weresignificantly different both in the dry season and in the wet season. In addition to Hedi,Nanshui, Fengshuba, Tiegang and Tangxi Reservoir, the N2O saturations of otherreservoirs were all lower in the surface water than in the bottom water (P<0.01), hadlayered phenomenon. The N2O saturations of the surface water and bottom water inreservoirs had no significant relationships (P>0.01) in dry season. Depositconcentration compared with other waters, N2O saturations of reservoirs and theirinput rivers were over-saturationed.N2O water-atmosphere fluxes were estimated by the Liss&Meriivat (1986)and Wanninkhof (1992) formula. The results demonstrated that reservoirs and theirinput rivers kept lower N2O water-atmosphere fluxes in wet season than dry season,with significant seasonal variations (P<0.01). Seeing from Spatial variation, changingtrends of N2O water-atmosphere fluxes was Pearl Delta area> Dongjiang watershed>Coastal area in west Guangdong> Coastal area in east Guangdong> Beijiangwatershed. Based on the reservoir surface area and average annual N2O flux, theannual N2O emission from the studied area was about3.88×10-5Tg·a-1, account for0.0037%of the total N2O emissions of China.Make analysis between N2O concentration, saturations, water-atmosphere fluxes and water physical and chemical characteristics,The correlation analysis suggestingthat in the wet season, inorganic nitrogen, were key factors to affect the produce anddistribution of N2O, which were also affected by factors such as temperature,dissolved oxygen, pH and chlorophyll in the dry season.
Keywords/Search Tags:reservoirs, input rivers, nitrous oxide, concentrations, distribution, flux, spatiotemporal variation
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