4.7 Article

Influence of water table level and soil properties on emissions of greenhouse gases from cultivated peat soil

期刊

SOIL BIOLOGY & BIOCHEMISTRY
卷 43, 期 5, 页码 923-931

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2011.01.002

关键词

Peat soils; Greenhouse gas emission; Groundwater level; Agricultural soils; Lysimeter; CO(2); Organic soils

资金

  1. European Union [EUROPEAT QLK5-CT-2002-01835]

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A lysimeter method using undisturbed soil columns was used to investigate the effect of water table depth and soil properties on soil organic matter decomposition and greenhouse gas (GHG) emissions from cultivated peat soils. The study was carried out using cultivated organic soils from two locations in Sweden: Orke, a typical cultivated fen peat with low pH and high organic matter content and Majne-garden, a more uncommon fen peat type with high pH and low organic matter content. Even though carbon and nitrogen contents differ greatly between the sites, carbon and nitrogen density are quite similar. A drilling method with minimal soil disturbance was used to collect 12 undisturbed soil monoliths (50 cm high, 029.5 cm) per site. They were sown with ryegrass (Lolium perenne) after the original vegetation was removed. The lysimeter design allowed the introduction of water at depth so as to maintain a constant water table at either 40 cm or 80 cm below the soil surface. CO(2), CH(4) and N(2)O emissions from the lysimeters were measured weekly and complemented with incubation experiments with small undisturbed soil cores subjected to different tensions (5, 40. 80 and 600 cm water column). CO(2) emissions were greater from the treatment with the high water table level (40 cm) compared with the low level (80 cm). N(2)O emissions peaked in springtime and CH(4) emissions were very low or negative. Estimated GHG emissions during one year were between 2.70 and 3.55 kg CO(2) equivalents m(-2). The results from the incubation experiment were in agreement with emissions results from the lysimeter experiments. We attribute the observed differences in GHG emissions between the soils to the contrasting dry matter liability and soil physical properties. The properties of the different soil layers will determine the effect of water table regulation. Lowering the water table without exposing new layers with easily decomposable material would have a limited effect on emission rates. (C) 2011 Elsevier Ltd. All rights reserved.

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