Nitrous oxide emissions from an irrigated sandy-clay loam cropped to maize and wheat

被引:0
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作者
T. Mahmood
R. Ali
K. A. Malik
S. R. A. Shamsi
机构
[1] Soil Biology Division,
[2] Nuclear Institute for Agriculture and Biology,undefined
[3] P. O. Box 128,undefined
[4] Faisalabad,undefined
[5] Pakistan Fax: +92-041-654213,undefined
[6] National Institute for Biotechnology and Genetic Engineering,undefined
[7] P. O. Box 577,undefined
[8] Faisalabad,undefined
[9] Pakistan,undefined
[10] Department of Botany,undefined
[11] University of the Punjab,undefined
[12] Quaid-e-Azam Campus,undefined
[13] Lahore,undefined
[14] Pakistan,undefined
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Key words Irrigation; Maize; Nitrous oxide; Urea; Wheat;
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摘要
 Nitrous oxide (N2O) emissions were measured from an irrigated sandy-clay loam cropped to maize and wheat, each receiving urea at 100 kg N ha–1. During the maize season (24 August–26 October), N2O emissions ranged between –0.94 and 1.53 g N ha–1 h–1 with peaks during different irrigation cycles (four) ranging between 0.08 and 1.53 g N ha–1 h–1. N2O sink activity during the maize season was recorded on 10 of the 29 sampling occasions and ranged between 0.18 and 0.94 g N ha–1 h–1. N2O emissions during the wheat season (22 November–20 April) varied between –0.85 and 3.27 g N ha–1 h–1, whereas peaks during different irrigation cycles (six) were in the range of 0.05–3.27 g N ha–1 h–1. N2O sink activity was recorded on 14 of the 41 samplings during the wheat season and ranged between 0.01 and 0.87 g N ha–1 h–1. Total N2O emissions were 0.16 and 0.49 kg N ha–1, whereas the total N2O sink activity was 0.04 and 0.06 kg N ha–1 during the maize and wheat seasons, respectively. N2O emissions under maize were significantly correlated with denitrification rate and soil NO3–-N but not with soil NH4+-N or soil temperature. Under wheat, however, N2O emissions showed a strong correlation with soil NH4+-N, soil NO3–-N and soil temperature but not with the denitrification rate. Under either crop, N2O emissions did not show a significant relationship with water-filled pore space or soil respiration.
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页码:189 / 196
页数:7
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