WANG Yu-Ying, HU Chun-Sheng. Soil greenhouse gas emission in winter wheat/summer maize rotation ecosystem as affected by nitrogen fertilization in the Piedmont Plain of Mount Taihang, China[J]. Chinese Journal of Eco-Agriculture, 2011, 19(5): 1122-1128. DOI: 10.3724/SP.J.1011.2011.01122
Citation: WANG Yu-Ying, HU Chun-Sheng. Soil greenhouse gas emission in winter wheat/summer maize rotation ecosystem as affected by nitrogen fertilization in the Piedmont Plain of Mount Taihang, China[J]. Chinese Journal of Eco-Agriculture, 2011, 19(5): 1122-1128. DOI: 10.3724/SP.J.1011.2011.01122

Soil greenhouse gas emission in winter wheat/summer maize rotation ecosystem as affected by nitrogen fertilization in the Piedmont Plain of Mount Taihang, China

  • The effect of soil nutrient augmentation via nitrogen deposition or fertilization on the processes of storing, releasing and re-absorbing of methane (CH4) carbon dioxide (CO2) and nitrous oxide (N2O) greenhouse gases (GHG) in soil ecosystems are poorly understood. This study described an original field experiment for measuring soil GHG flux at nitrogen application rates of N0 0 kg(N)·hm-2, N200 200 kg(N)·hm-2, N400 400 kg(N)·hm-2and N600 600 kg(N)·hm-2 in winter wheat/summer maize double cropping system in the Piedmont Plains of Mount Taihang. CH4, CO2 and N2O emissions from soils under the winter wheat/summer maize rotation system were measured from July 2008 through June 2010 using the static transparent chamber and gas chromatography technique. The results showed that soils under winter wheat/summer maize ecosystems served as CH4 sink, and CO2 and N2O sources. With increasing nitrogen application, CH4 absorption rate decreased and CO2 and N2O flux rates increased. In winter wheat season, CH4 absorption rate under N0 treatment was significantly higher than under other nitrogen treatments. Both CO2 and N2O emission flux rates under N600 treatment were significantly higher (P<0.05) than under N0 treatment. Nitrogen fertilization and irrigation sharply induced CO2 and N2O peak flux emissions and decreased CH4 peak absorption. Rising soil temperature, precipitation or alternating wet/dry weather increased soil N2O and CO2 emission flux rates. Negative N2O flux rates were observed under low temperature and high evaporation conditions in N0 application treatments in winter. CH4 emission accumulation for 2008~2009 under N0, N200, N400 and N600 treatments was -1.42, -0.75, -0.82 and -0.92 kg·hm-2·a-1, respectively. For 2009~2010, it was -2.60, -1.47, -1.35 and -1.76 kg·hm-2·a-1, respectively. CO2 emission accumulation for 2008~2009 under N0, N200, N400 and N600 treatments was 15 598, 19 346, 21 456 and 29 013 kg·hm-2·a-1, respectively. For 2009~2010, it was 10 318, 11 474, 13 984 and 20 639 kg·hm-2·a-1, respectively. Then N2O emission accumulation for 2008~2009 under N0, N200, N400 and N600 treatments was 1.05, 2.16, 5.27 and 6.98 kg·hm-2·a-1, respectively. Also for 2009~2010, it was 1.49, 2.31, 4.42 and 5.81 kg·hm-2·a-1, respectively.
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