FENG Xiaoming, WANG Kai, ZHENG Xunhua, LUO Xianbao, WANG Rui, WANG Dong. Net methane flux exchange in subtropical vegetable fields[J]. Chinese Journal of Eco-Agriculture, 2018, 26(8): 1091-1099. DOI: 10.13930/j.cnki.cjea.180187
Citation: FENG Xiaoming, WANG Kai, ZHENG Xunhua, LUO Xianbao, WANG Rui, WANG Dong. Net methane flux exchange in subtropical vegetable fields[J]. Chinese Journal of Eco-Agriculture, 2018, 26(8): 1091-1099. DOI: 10.13930/j.cnki.cjea.180187

Net methane flux exchange in subtropical vegetable fields

  • Agricultural soil forms an important source-sink of atmospheric methane (CH4). Studies on net CH4 flux exchange in agricultural soil have mainly been related to rice, wheat, maize and other crops. However, field studies on vegetable fields have been seldom reported. This study was a year-round situ measurement of CH4 flux in a typical subtropical vegetable field cultivated with cabbages using the static chamber/gas chromatography technique. The aims were to determine the characteristics of annual net exchange flux of CH4 and the influencing factors, to estimate annual cumulative CH4 flux, and to quantify errors in measured CH4 flux. The CH4 flux measurements were conducted on ridges and on inter-ridges in vegetable fields for period from January 1st to December 8th 2016. Environmental conditions were simultaneously observed during the measurement period. The results showed that vegetable fields constituted a weak sink of atmospheric CH4, with annual mean flux of (-9.9±7.0) μg(C)·m-2·h-1 and annual cumulative flux of -0.84 kg(C)·hm-2. High soil water content and nitrogen fertilizer application rate were probably the main reasons for the weak uptake of CH4. The overall error in the annual cumulative CH4 flux was -48%——16%. The main source of systematic error was in the flux calculation method used, which underestimated the flux by 32% on average. Random error was mainly produced by spatial variations of CH4 flux, which was estimated at 16% at annual time scale. As a result, it was recommended that high numbers of spatial replications were used in conducting greenhouse gas flux measurements in agricultural soil in order to reduce random error. Another finding of the study was that CH4 uptake measured on the ridge was significantly (P < 0.01) larger than that measured on the inter-ridge. This implied that it was better to simultaneously place chambers on areas with different field management practices; e.g. ridge and inter-ridge, row and inter-row, which efficiently avoided systematic error in measured flux.
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