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Taylor and Francis Group, Soil Science and Plant Nutrition, 4(53), p. 362-372, 2007

DOI: 10.1111/j.1747-0765.2007.00152.x

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Time-lagged induction of N2O emission and its trade-off with NO emission from a nitrogen fertilized Andisol

Journal article published in 2007 by Weixin Ding, Kazuyuki Yagi, Hiroko Akiyama, Shigeto Sudo ORCID, Seiichi Nishimura
This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Abstract

To understand the influence of basal application of N fertilizer on nitrification potential and N2O and NO emissions, four soil samples were collected from an upland Andisol field just before (sample 1) and 4 (sample 2), 36 (sample 3) and 72 (sample 4) days after the basal application of N fertilizer during the Chinese cabbage growing season from 12 September to 30 November 2005. The potentials of N2O production and nitrification of the soils were determined using a N tracer technique and the soils were incubated for 25 days at 25°C and 60% water-filled pore space (WFPS). The results revealed that as much as 84–97% N2O and almost all NO were produced by nitrification. The N2O emission peak occurred approximately 350 h after the beginning of incubation for samples 1 and 2, but just 48 h later in samples 3 and 4. Total N2O emission during the 25-day incubation of samples 3 and 4 ranged from 190 to 198 µg N kg soil, which was significantly higher than the 99–108 µg N kg soil recorded in samples 1 and 2. Basal application of N fertilizer did not immediately increase the nitrification potential and the ratio of N2O to N added, but did dramatically increase the nitrification potential and the ratio of N2O to N added as (NH4)2SO4 36–72 days after the basal N fertilizer was added. In contrast, NO emission was negatively correlated with nitrification potential and total N2O emission. As a result, a trade-off relationship between total NO and N2O emissions was identified. The results indicated that there was a time-lagged induction of the change of N turnover in the soil, which was possibly caused by slow population growth of the nitrifiers and/or a slow shift in the microbial community in the soil.