Soil–atmosphere greenhouse gas exchange in a cool, temperate Eucalyptus delegatensis

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• 作者：Benedikt J. Fest ; Stephen J. Livesley ; Matthias Drö ; sler ; Eva van Gorsel ; Stefan K. Arndt
• 关键词：Acacia dealbata ; Eucalyptus delegatensis ; Forest soil ; Greenhouse gases ; Methane ; Nitrous oxide ; Nitrogen fixing
• 刊名：Agricultural and Forest Meteorology
• 出版年：2009
• 出版时间：11 March 2009
• 年：2009
• 卷：149
• 期：3-4
• 页码：393-406
• 全文大小：1041 K

文摘

Forests are the largest C sink (vegetation and soil) in the terrestrial biosphere and may additionally provide an important soil methane (CH₄) sink, whilst producing little nitrous oxide (N₂O) when nutrients are tightly cycled. In this study, we determine the magnitude and spatial variation of soil–atmosphere N₂O, CH₄ and CO₂ exchange in a Eucalyptus delegatensis forest in New South Wales, Australia, and investigate how the magnitude of the fluxes depends on the presence of N₂-fixing tree species (Acacia dealbata), the proximity of creeks, and changing environmental conditions. Soil trace gas exchange was measured along replicated transects and in forest plots with and without presence of A. dealbata using static manual chambers and an automated trace gas measurement system for 2 weeks next to an eddy covariance tower measuring net ecosystem CO₂ exchange. CH₄ was taken up by the forest soil (−51.8 μg CH₄-C m⁻² h⁻¹) and was significantly correlated with relative saturation (S_r) of the soil. The soil within creek lines was a net CH₄ source (up to 33.5 μg CH₄-C m⁻² h⁻¹), whereas the wider forest soil was a CH₄ sink regardless of distance from the creek line. Soil N₂O emissions were small (<3.3 μg N₂O-N m⁻² h⁻¹) throughout the 2-week period, despite major rain and snowfall. Soil N₂O emissions only correlated with soil and air temperature. The presence of A. dealbata in the understorey had no influence on the magnitude of CH₄ uptake, N₂O emission or soil N parameters. N₂O production increased with increasing soil moisture (up to 50 % S_r) in laboratory incubations and gross nitrification was negative or negligible as measured through ¹⁵N isotope pool dilution.

The small N₂O emissions are probably due to the limited capacity for nitrification in this late successional forest soil with C:N ratios >20. Soil–atmosphere exchange of CO₂ was several orders of magnitude greater (88.8 mg CO₂-C m⁻² h⁻¹) than CH₄ and N₂O, and represented 43 % of total ecosystem respiration. The forest was a net greenhouse gas sink (126.22 kg CO₂-equivalents ha⁻¹ d⁻¹) during the 2-week measurement period, of which soil CH₄ uptake contributed only 0.3 % and N₂O emissions offset only 0.3 % .