Soil N 2 O Emissions under Different N Rates in an Oil Palm Plantation on Tropical Peatland
Auldry Chaddy,
Lulie Melling,
Kiwamu Ishikura and
Ryusuke Hatano
Additional contact information
Auldry Chaddy: Laboratory of Soil Science, Graduate School of Agriculture, Hokkaido University, Hokkaido 060-8589, Japan
Lulie Melling: Sarawak Tropical Peat Research Institute, Lot 6035, Kuching-Samarahan Expressway, 94300 Kota Samarahan, Sarawak, Malaysia
Kiwamu Ishikura: Tokachi Agricultural Experiment Station, Hokkaido Research Organization, Hokkaido 082-0081 Japan
Ryusuke Hatano: Laboratory of Soil Science, Graduate School of Agriculture, Hokkaido University, Hokkaido 060-8589, Japan
Agriculture, 2019, vol. 9, issue 10, 1-18
Abstract:
(1) Background: Nitrogen (N) fertilization on drained tropical peatland will likely stimulate peat decomposition and mineralization, enhancing N 2 O emission from the peat soil. (2) Methods: A field experiment was conducted to quantify the N 2 O emissions from soil in an oil palm plantation ( Elaeis guineensis Jacq.) located in a tropical peatland in Sarawak, Malaysia, under different rates of N fertilizers. The study was conducted from January 2010 to December 2013 and resumed from January 2016 to December 2017. Nitrous oxide (N 2 O) flux was measured every month using a closed chamber method for four different N rates; control—without N (T1), 31.1 kg N ha −1 yr −1 (T2), 62.2 kg N ha −1 yr −1 (T3), and 124.3 kg N ha −1 yr −1 (T4); (3) Results: Application of the N fertilizer significantly increased annual cumulative N 2 O emissions for T4 only in the years 2010 ( p = 0.017), 2011 ( p = 0.012), 2012 ( p = 0.007), and 2016 ( p = 0.048). The highest average annual cumulative N 2 O emissions were recorded for T4 (41.5 ± 28.7 kg N ha −1 yr −1 ), followed by T3 (35.1 ± 25.7 kg N ha −1 yr −1 ), T1 (25.2 ± 17.8 kg N ha −1 yr −1 ), and T2 (25.1 ± 15.4 kg N ha −1 yr −1 ), indicating that the N rates of 62.2 kg N ha −1 yr −1 and 124.3 kg N ha −1 yr −1 increased the average annual cumulative N 2 O emissions by 39% and 65%, respectively, as compared to the control. The N fertilization had no significant effect on annual oil palm yield ( p = 0.994). Alternating between low (deeper than −60 cm) and high groundwater level (GWL) (shallower than −60 cm) enhanced nitrification during low GWL, further supplying NO 3 − for denitrification in the high GWL, and contributing to higher N 2 O emissions in high GWL. The emissions of N 2 O ranged from 17 µg N m −2 hr −1 to 2447 µg N m −2 hr −1 and decreased when the water-filled pore space (WFPS) was between 70% and 96%, suggesting the occurrence of complete denitrification. A positive correlation between N 2 O emissions and NO 3 − at 70–96% WFPS indicated that denitrification increased with increased NO 3 − availability. Based on their standardized regression coefficients, the effect of GWL on N 2 O emissions increased with increased N rate ( p < 0.001). Furthermore, it was found that annual oil palm yields negatively correlated with annual N 2 O emission and NO 3 − for all treatments. Both nitrification and denitrification increased with increased N availability, making both processes important sources of N 2 O in oil palm cultivation on tropical peatland.; and (4) Conclusions: To improve understanding of N 2 O mitigation strategies, further studies should consider plant N uptake on N 2 O emissions, at least until the completion of the planting.
Keywords: ground water level (GWL); water-filled pore space (WFPS); oil palm yield; nitrification; denitrification (search for similar items in EconPapers)
JEL-codes: Q1 Q10 Q11 Q12 Q13 Q14 Q15 Q16 Q17 Q18 (search for similar items in EconPapers)
Date: 2019
References: View complete reference list from CitEc
Citations: View citations in EconPapers (1)
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