Substantial N2O emissions from peat decomposition and N fertilization in an oil palm plantation exacerbated by hotspots. (4th October 2017)

• Record Type: Journal Article
• Authors: Oktarita, Satria; Hergoualc'h, Kristell; Anwar, Syaiful; Verchot, Louis V
• Is Part Of: Environmental research letters. Volume 12:Number 10(2017:Oct.)
• Publication Date: 2017-10-04
• Subjects: global warming -- greenhouse gases -- nitrous oxide -- nitrification -- mineralization -- fertilizer -- tropical peatland; Environmental sciences -- Periodicals; Human ecology -- Research -- Periodicals; Environmental health -- Periodicals; 333.7
• DOI: 10.1088/1748-9326/aa80f1
• Languages: English
• ISSNs: 1748-9326

Abstract

Abstract: It is unclear to what extent emissions of nitrous oxide (N2 O) from drained histosols in the tropics may contribute to the atmospheric burden of greenhouse gases. In particular, there is a critical need to elucidate their magnitude in oil palm plantations on these soils. We examined spatio-temporal variations of N2 O emissions from peat decomposition and nitrogen (N) fertilization in a plantation trial in Sumatra, which included three application rates: 0 (N0), 153 (N1) and 306 (N2) kg N ha −1 y −1 . The spatially stratified sampling design distinguished the area around the palms which received fertilizer (9% of the surface) from the rest of the plot which was unfertilized. Annual emissions were substantial with rates of 22.1 ± 5.7, 12.8 ± 2.7 and 26.6 ± 5.7 kg N2 O-N ha −1 in the N0, N1 and N2 treatments, respectively. These equal 9.3 ± 2.4, 5.4 ± 1.1 and 11.2 ± 2.4 Mg CO2 eq ha −1 y −1, or 5–10 times emission rates in natural peatland forest. The site exhibited two persistent hotspots located in the unfertilized zone, contributing 33 and 46% of annual emissions in N0 and N2 while representing only 10% of the area sampled. The response of emissions to fertilization was exponential but restricted to the small N application area. At the plot scale and over the year, the impact of fertilized-induced emissions was minimal due to the prevalence of emissions from peat decomposition. Annual rates among treatments were similar when discarding the contribution of hotspots to evaluate N addition effect. High N2 O emissions from peat decomposition in the tropics tend to be common within the restricted existing literature; which is in contrast with most recent IPCC emission factors. Our results emphasize the importance to integrate N2 O emissions in greenhouse gas budgets of plantations on peat, despite the predominance of CO2 in total emissions.