No Wildfire Legacy Effect on Peat Carbon Stability Under Severe Drought in a Lowland Peat Mosaic

IF 4.3 2区 农林科学 Q2 SOIL SCIENCE
Keunbae Kim, Willem-Jan Emsens, Judith Schellekens, Erik Verbruggen, Bas Van der Veken, Layla Maas, Rudy van Diggelen, María J. I. Briones, Boris Jansen, Karen Vancampenhout
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Abstract

Ongoing climate change, particularly warmer and drier conditions, disrupts hydrological stability in peatland ecosystems and elevates wildfire risk. Higher burn severity and frequency are expected to accelerate carbon (C) losses and amplify climate-carbon feedback. In this study, we used an accidental and short-lived wildfire that occurred in 2020 at Landschap De Liereman (Belgium), a mosaic landscape ranging from poor-fen to bog-like peatlands, to investigate how belowground C dynamics respond to peatland fire in the subsequent four consecutive years under ongoing climatic pressures. A paired plot design was established, consisting of burnt and nearby intact plots, based on field measurements in combination with remote sensing data. Burnt peatland patches with no smoldering fire were significantly altered during the first 2 years after the fire, evidenced by a lower topsoil C:N ratios, reduced C and N isotopic values (Ps < 0.05), and shifts in soil organic matter (SOM) composition. Especially, carbohydrates declined whereas benzenes and N compounds increased (p < 0.05), indicating depletion of labile C and accumulation of recalcitrant aromatic C leading to lower soil organic carbon (SOC) decomposability (i.e., basal respiration per unit peat C, p < 0.05). These differences diminished within 3 years, with very little changes in bulk soil C and N contents between intact and burnt plots, suggesting a relatively high resilience to a low-severity fire. However, in 2022, abrupt changes in soil C and N concentrations, SOM composition, and SOC decomposability were observed in all paired plots, regardless of whether they were affected by the fire, and that were likely related to drought stress, as 2022 was an exceptionally dry year. The damage of this drought was substantial, but not different between intact and burnt plots, indicating that there was no fire legacy effect on soil components and C stability in surface peat.

严重干旱下低地泥炭嵌合区野火遗产对泥炭碳稳定性的影响
持续的气候变化,特别是温暖和干燥的条件,破坏了泥炭地生态系统的水文稳定性,增加了野火的风险。更高的燃烧强度和频率预计会加速碳(C)的损失,并放大气候-碳反馈。在这项研究中,我们利用2020年发生在Landschap De Liereman(比利时)的一场意外的、短暂的野火,研究了在持续的气候压力下,连续四年地下碳动力学对泥炭地火灾的响应。Landschap De Liereman是一个从贫瘠沼泽到沼泽状泥炭地的马赛克景观。基于野外测量和遥感数据,建立了由烧毁样地和附近完整样地组成的成对样地设计。未发生阴燃火灾的泥炭地斑块在火灾后的前2年内发生了显著变化,表现为表层土壤C:N比降低,C和N同位素值降低(p < 0.05),土壤有机质(SOM)组成发生了变化。特别是碳水化合物减少,而苯类和氮类化合物增加(p < 0.05),表明土壤中挥发性碳的消耗和顽固性芳香碳的积累导致土壤有机碳(SOC)分解能力(即单位泥炭碳的基础呼吸,p < 0.05)降低。这些差异在3年内逐渐消失,原状和烧毁地块的土壤C和N含量变化很小,表明对低严重度火灾的恢复能力相对较高。然而,在2022年,无论是否受到火灾的影响,所有配对样地的土壤C和N浓度、SOM组成和有机碳分解能力都发生了突变,这可能与干旱胁迫有关,因为2022年是一个异常干旱的年份。此次干旱造成的破坏是巨大的,但在完整地和烧毁地之间没有差异,表明火灾对土壤成分和地表泥炭碳稳定性没有影响。
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来源期刊
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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