Determination of methane and carbon dioxide fluxes during the rice maturity period in Taiwan by combining profile and eddy covariance measurements
Determination of methane and carbon dioxide fluxes during the rice maturity period in Taiwan by combining profile and eddy covariance measurements
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DOI:
10.1016/j.agrformet.2010.04.007
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发表时间:
2010-06
影响因子:
6.2
通讯作者:
K. Tseng;Jeng-Lin Tsai;A. Alagesan;B. Tsuang;M. Yao;Pei-Hsuan Kuo
中科院分区:
文献类型:
--
作者:
K. Tseng;Jeng-Lin Tsai;A. Alagesan;B. Tsuang;M. Yao;Pei-Hsuan Kuo
A field campaign was undertaken over a rice paddy in Central Taiwan to investigate the flux of CH4through the flux-gradient method. During the campaign period, the average observed concentrations of CH4during the campaign period at the lower height (22.2m above ground level, agl) and upper height (27.5magl) were around 2.04ppm and 2.01ppm, respectively. It was noticed that the profile concentration of CH4was lower during day time when compared to night time. However, the flux of CH4was observed to be higher during the day time than during night hours. In order to understand the relationship between the influences of meteorological variables on the flux of CH4, six meteorological variables were studied. It was observed that soil heat flux has a linear positive correlation with the flux of CH4. During the study period, the maturity stage of rice paddy, the rice paddy ecosystem was behaving as sources of CH4and CO2. Over a 100-year time frame, the global warming potential (GWP) fluxes of CH4and CO2observed at this study site were 0.16 and 0.71μmolCO2equivalentsm−2s−1, respectively.The total GWP flux (CH4and CO2) was 0.86μmolCO2equivalentsm−2s−1in which CH4and CO2contribute 18% and 82%, respectively.