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Soil N 2 O Emissions under Different N Rates in an Oil Palm Plantation on Tropical Peatland

机译:热带泥炭地油棕人工林不同氮素养分下的土壤N 2 O排放

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(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.
机译:(1)背景:在流失的热带泥炭地施氮(N)可能会刺激泥炭分解和矿化,增加泥炭土壤中N 2 O的排放。 (2)方法:进行了田间试验,以定量研究了在马来西亚砂拉越热带泥炭地的油棕种植园(Elaeis guineensis Jacq。)中,不同氮肥用量下土壤中N 2 O的排放量。该研究于2010年1月至2013年12月进行,并于2016年1月至2017年12月恢复。每月使用密闭室法对四种不同的N速率测量一氧化二氮(N 2 O)通量。对照—无N(T1),31.1kg N ha≤1yr≤1(T3),62.2kg N ha≤1yr≤1(T3)和124.3kg N ha≤1yr≤1(T4); (3)结果:仅在2010年(p = 0.017),2011年(p = 0.012),2012年(p = 0.007)和2016年(p = 0.048)。 T4(41.5±28.7 kg N ha·1 yr·1)的最高平均年累积N 2 O排放量,其次是T3(35.1±25.7 kg N ha·1 yr·1),T1(25.2±17.8 kg N ha?1 yr?1)和T2(25.1±15.4 kg N ha?1 yr?1)表示N比率分别为62.2 kg N ha?1 yr?1和124.3 kg N ha?1 yr?1。与对照组相比,平均年累积N 2 O排放分别增加了39%和65%。施氮对油棕的年产量无显着影响(p = 0.994)。在低(GWL)低(深度小于60 cm)和高地下水位(GWL)(小于60 cm)之间交替进行可增强硝化作用,进一步提供NO 3?用于高GWL中的反硝化,并有助于高GWL中较高的N 2 O排放。 N 2 O的排放量在17μgN m?2 hr?1到2447μgN m?2 hr?1的范围内,并在充满水的孔隙空间(WFPS)在70%至96%之间时降低。完全脱氮。 N 2 O排放与NO 3?之间呈正相关。 WFPS为70–96%时,表明反硝化随NO 3的增加而增加。可用性。基于他们的标准化回归系数,GWL对N 2 O排放的影响随着N率的增加而增加(p <0.001)。此外,还发现年油棕产量与年N 2 O排放和NO 3?负相关。适用于所有治疗。随着氮素利用率的提高,硝化作用和反硝化作用均增加,这两个过程均成为热带泥炭地油棕种植过程中N 2 O的重要来源。 (4)结论:为增进对N 2 O缓解策略的理解,进一步的研究应考虑植物吸收N 2 O的氮吸收量,至少要等到种植完成为止。

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