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  Soil carbon inventories and carbon-13 on a latitude transect in Siberia

Bird, M. I., Santrùcková, H., Arneth, A., Grigoriev, S., Gleixner, G., Kalaschnikov, Y. N., Lloyd, J., & Schulze, E.-D. (2002). Soil carbon inventories and carbon-13 on a latitude transect in Siberia. Tellus, Series B - Chemical and Physical Meteorology, 54(5), 631-641. doi:10.1034/j.1600-0889.2002.01334.x.

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資料種別: 学術論文

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BGC0444.pdf (出版社版), 271KB
 
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 作成者:
Bird, M. I., 著者
Santrùcková, H., 著者
Arneth, A.1, 著者           
Grigoriev, S., 著者
Gleixner, G.2, 著者           
Kalaschnikov, Y. N., 著者
Lloyd, J.3, 著者           
Schulze, E.-D.1, 著者           
所属:
1Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497751              
2Molecular Biogeochemistry Group, Dr. G. Gleixner, Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497773              
3Research Group Carbon-Change Atmosphere, Dr. J. Lloyd, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497762              

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キーワード: Microbial processes; forest ecosystems; CO2; discrimination; delta-c-13; biosphere; ratio
 要旨: We present soil organic carbon (SOC) inventories and carbon isotope compositions from over 900 samples collected in areas of minimally disturbed mature vegetation on freely drained soils (excluding peatlands) on a 1000 km transect along the Yennisey River, central Siberia. Carbon inventories over 0-30 cm depth range widely from 1.71 to 7.05 kg m(-2). While an effect of changing climate or vegetation along the transect cannot be ruled out, the observed differences in SOC inventories are largely the result of variations in mineral soil texture, with inventories in fine-textured soils being approximately double those in coarse-textured soils. The delta(13)C values of SOC in the 0-5 cm interval ranged from - 26.3 to -28.0parts per thousand, with delta(13)C values for the 5-30 cm interval being 0.9 +/- 0.8parts per thousand (1sigma) enriched in C-13 relative to the 0-5 cm samples. The average delta(13)C value for the 0-5 cm interval for all samples was - 27.1 +/- 0.6parts per thousand (1sigma) and for the full 0-30 cm interval the average was -26.5 +/- 0.5parts per thousand (1sigma). In general, delta(13)C values were higher in coarse- textured soils and lower in fine-textured soils. The results of detailed sampling of soils in Pinus sylvestris forest growing on sand near the Zotino flux tower suggest an SOC inventory in these soils of 2.22 +/- 0.35 kg m(-2) over 30 cm and an average delta(13)C value of -26.3 +/- 0.2parts per thousand over the 0- 5 cm depth interval and -25.9 +/- 0.3parts per thousand over 0- 30 cm. Recent burning had no effect on SOC inventories, but clearing has led to an average 25% decrease on SOC inventories from 0-30 cm over 12 yr. Neither burning nor clearing had a discernible effect on the delta(13)C value of SOC.

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 日付: 2002
 出版の状態: 出版
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 識別子(DOI, ISBNなど): その他: BGC0444
DOI: 10.1034/j.1600-0889.2002.01334.x
PII: 393
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出版物 1

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出版物名: Tellus, Series B - Chemical and Physical Meteorology
種別: 学術雑誌
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出版社, 出版地: Copenhagen : Swedish Geophysical Society :
ページ: - 巻号: 54 (5) 通巻号: - 開始・終了ページ: 631 - 641 識別子(ISBN, ISSN, DOIなど): CoNE: https://pure.mpg.de/cone/journals/resource/954925506308
ISSN: 0280-6509