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Carbon dynamics in a temperate grassland soil after 9 years exposure to elevated CO2 (Swiss FACE)

文献类型:期刊论文

作者Xie, ZB; Cadisch, G; Edwards, G; Baggs, EM; Blum, H
刊名SOIL BIOLOGY & BIOCHEMISTRY
出版日期2005-07-01
卷号37期号:7页码:1387-1395
关键词elevated CO2 Swiss FACE carbon sequestration C-13 soil fractionation priming effect CO2 emission
ISSN号0038-0717
DOI10.1016/j.soilbio.2004.12.010
通讯作者Xie, ZB()
英文摘要Elevated pCO(2) increases the net primary production, C/N ratio, and C input to the soil and hence provides opportunities to sequester CO2-C in soils to mitigate anthropogenic CO2. The Swiss 9 y grassland FACE (free air carbon-dioxide enrichment) experiment enabled us to explore the potential of elevated pCO(2) (60 Pa), plant species (Lolium perenne L. and Trifolium repens L.) and nitrogen fertilization (140 and 540 kg ha(-1) y(-1)) on carbon sequestration and mineralization by a temperate grassland soil. Use of C-13 in combination with respired CO2 enabled the identification of the origins of active fractions of soil organic carbon. Elevated pCO(2) had no significant effect on total soil carbon, and total soil carbon was also independent of plant species and nitrogen fertilization. However, new (FACE-derived depleted C-13) input of carbon into the soil in the elevated pCO(2) treatments was dependent on nitrogen fertilization and plant species. New carbon input into the top 15 cm of soil from L. perennne high nitrogen (LPH), L. perenne low nitrogen (LPL) and T. repens low nitrogen (TRL) treatments during the 9 y elevated pCO(2) experiment was 9.3 &PLUSMN; 2.0, 12.1 &PLUSMN; 1.8 and 6.8 &PLUSMN; 2.7 Mg C ha(-1), respectively. Fractions of FACE-derived carbon in less protected soil particles > 53 μ m in size were higher than in < 53 μ m particles. In addition, elevated pCO(2) increased CO2 emission over the 118 d incubation by 55, 61 and 13% from undisturbed soil from LPH, LPL and TRL treatments, respectively; but only by 13, 36, and 18%, respectively, from disturbed soil (without roots). Higher input of new carbon led to increased decomposition of older soil organic matter (priming effect), which was driven by the quantity (mainly roots) of newly input carbon (L. perenne) as well as the quality of old soil carbon (e.g. higher recalcitrance in T. repens). Based on these results, the potential of well managed and established temperate grassland soils to sequester carbon under continued increasing concentrations of atmospheric CO2 appears to be rather limited. © 2005 Elsevier Ltd. All rights reserved.
收录类别SCI
WOS关键词ATMOSPHERIC CO2 ; ORGANIC-MATTER ; DECOMPOSITION ; INPUT ; C-13 ; ENRICHMENT ; DIOXIDE ; SEQUESTRATION ; BIOMASS ; SWARDS
WOS研究方向Agriculture
WOS类目Soil Science
语种英语
WOS记录号WOS:000229514600016
出版者PERGAMON-ELSEVIER SCIENCE LTD
URI标识http://www.irgrid.ac.cn/handle/1471x/2558463
专题南京土壤研究所
通讯作者Xie, ZB
作者单位1.Chinese Acad Sci, Inst Soil Sci, State Key Lab Soils & Sustainable Agr, Nanjing 210008, Peoples R China
2.Univ London Imperial Coll Sci Technol & Med, Dept Agr Sci, Ashford TN25 5AH, Kent, England
3.Univ Aberdeen, Sch Biol Sci, Aberdeen AB24 3UU, Scotland
4.ETH, Inst Plant Sci, CH-8092 Zurich, Switzerland
5.Lincoln Univ, Agr & Life Sci Div, Canterbury, New Zealand
推荐引用方式
GB/T 7714
Xie, ZB,Cadisch, G,Edwards, G,et al. Carbon dynamics in a temperate grassland soil after 9 years exposure to elevated CO2 (Swiss FACE)[J]. SOIL BIOLOGY & BIOCHEMISTRY,2005,37(7):1387-1395.
APA Xie, ZB,Cadisch, G,Edwards, G,Baggs, EM,&Blum, H.(2005).Carbon dynamics in a temperate grassland soil after 9 years exposure to elevated CO2 (Swiss FACE).SOIL BIOLOGY & BIOCHEMISTRY,37(7),1387-1395.
MLA Xie, ZB,et al."Carbon dynamics in a temperate grassland soil after 9 years exposure to elevated CO2 (Swiss FACE)".SOIL BIOLOGY & BIOCHEMISTRY 37.7(2005):1387-1395.

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来源:南京土壤研究所

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