Thermal alteration of organic matter during a shrubland fire: A field study

被引:74
作者
Alexis, M. A. [1 ]
Rumpel, C. [1 ]
Knicker, H. [2 ]
Leifeld, J. [3 ]
Rasse, D. [4 ]
Pechot, N. [1 ]
Bardoux, G. [1 ]
Mariotti, A. [1 ]
机构
[1] Ctr INRA Versailles Grignon, Lab Biogeochim & Ecol Milieux Continentaux, F-78850 Thiverval Grignon, France
[2] Tech Univ Munich, Lehrstuhl Bodenkunde, D-85350 Freising Weihenstephan, Germany
[3] Swiss Fed Res Stn Agroecol & Agr, CH-8046 Zurich, Switzerland
[4] Norwegian Inst Agr & Environm Res, N-1432 As, Norway
关键词
C-13; CPMAS; CARBON; CHARCOAL; SOILS; WOOD; NITROGEN; FORESTS; PEAT; TRANSFORMATION; DECOMPOSITION;
D O I
10.1016/j.orggeochem.2010.03.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Vegetation fires profoundly alter the C cycle of terrestrial ecosystems, notably through the potential formation of highly stable pyrogenic structures. Fire-induced changes in the structure of organic matter (OM) have been studied mainly under controlled laboratory conditions. The objective of this work was to characterise changes in OM chemistry occurring in the litter layer of a scrub-oak ecosystem subjected to a prescribed fire. Maximum temperatures reached during the fire were monitored with thermo-sensitive paint. Litter samples collected before and after the fire were subjected to size fractionation, each size fraction being divided on the basis of visual observation into burnt and unburnt components, i.e. black and brown, respectively. All fractions were analysed for C and N contents and stable carbon isotopic composition. Shifts in the composition of >2 mm fraction components were evaluated using solid-state C-13 nuclear magnetic resonance (NMR) spectroscopy and differential scanning calorimetry (DSC). The effects of charring were evaluated through comparisons of black vs. brown post-fire litter in >370 degrees C plots. Comparison of bulk pre- vs. post-fire litter proved unreliable because of the complicating effect of fresh litter fall during the fire event. Charring significantly increased the litter C content by 115-142 mg g(-1) and significantly decreased the delta C-13 value by an average of 0.8 parts per thousand. The NMR and DSC analyses indicated that O-alkyl compounds were preferentially lost vs. aryl and alkyl compounds. This suggests a preferential loss of cellulose components and a relative preservation of lignin and lipids. However, the charred litter samples had a low degree of condensation vs. a graphitic-like model. The findings suggest that leaf-derived charcoal produced during natural vegetation fires does not contribute much to the highly stable fraction of pyrogenic OM. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:690 / 697
页数:8
相关论文
共 45 条
  • [11] Burning of Amazonian rainforests:: burning efficiency and charcoal formation in forest cleared for cattle pasture near Manaus, Brazil
    Fearnside, PM
    Graça, PMLD
    Rodrigues, FJA
    [J]. FOREST ECOLOGY AND MANAGEMENT, 2001, 146 (1-3) : 115 - 128
  • [12] Thermal resistance to high temperatures of different organic fractions from soils under pine forests
    Fernandez, I
    Cabaneiro, A
    Carballas, T
    [J]. GEODERMA, 2001, 104 (3-4) : 281 - 298
  • [13] 13C High-resolution solid-state NMR study of peat carbonization
    Freitas, JCC
    Bonagamba, TJ
    Emmerich, FG
    [J]. ENERGY & FUELS, 1999, 13 (01) : 53 - 59
  • [14] Spatial patterns of soil temperatures during experimental fires
    Gimeno-García, E
    Andreu, V
    Rubio, JL
    [J]. GEODERMA, 2004, 118 (1-2) : 17 - 38
  • [15] The heterogeneous nature of microbial products as shown by solid-state C-13 CP/MAS NMR spectroscopy
    Golchin, A
    Clarke, P
    Oades, JM
    [J]. BIOGEOCHEMISTRY, 1996, 34 (02) : 71 - 97
  • [16] Comparison of quantification methods to measure fire-derived (black/elemental) carbon in soils and sediments using reference materials from soil, water, sediment and the atmosphere
    Hammes, Karen
    Schmidt, Michael W. I.
    Smernik, Ronald J.
    Currie, Lloyd A.
    Ball, William P.
    Nguyen, Thanh H.
    Louchouarn, Patrick
    Houel, Stephane
    Gustafsson, Oerjan
    Elmquist, Marie
    Cornelissen, Gerard
    Skjemstad, Jan O.
    Masiello, Caroline A.
    Song, Jianzhong
    Peng, Ping'an
    Mitra, Siddhartha
    Dunn, Joshua C.
    Hatcher, Patrick G.
    Hockaday, William C.
    Smith, Dwight M.
    Hartkopf-Froeder, Christoph
    Boehmer, Axel
    Lueer, Burkhard
    Huebert, Barry J.
    Amelung, Wulf
    Brodowski, Sonja
    Huang, Lin
    Zhang, Wendy
    Gschwend, Philip M.
    Flores-Cervantes, D. Xanat
    largeau, ClauDe
    Rouzaud, Jean-Noeel
    Rumpel, Cornelia
    Guggenberger, Georg
    Kaiser, Klaus
    Rodionov, Andrei
    Gonzalez-Vila, Francisco J.
    Gonzalez-Perez, Jose A.
    de la Rosa, Jose M.
    Manning, David A. C.
    Lopez-Capel, Elisa
    Ding, Luyi
    [J]. GLOBAL BIOGEOCHEMICAL CYCLES, 2007, 21 (03)
  • [17] Synthesis and characterisation of laboratory-charred grass straw (Oryza saliva) and chestnut wood (Castanea sativa) as reference materials for black carbon quantification
    Hammes, Karen
    Smernik, Ronald J.
    Skjemstad, Jan O.
    Herzog, Andreas
    Vogt, Ulrich F.
    Schmidt, Michael W. I.
    [J]. ORGANIC GEOCHEMISTRY, 2006, 37 (11) : 1629 - 1633
  • [18] Global warming in the twenty-first century: An alternative scenario
    Hansen, J
    Sato, M
    Ruedy, R
    Lacis, A
    Oinas, V
    [J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2000, 97 (18) : 9875 - 9880
  • [19] Mineralisation and structural changes during the initial phase of microbial degradation of pyrogenic plant residues in soil
    Hilscher, Andre
    Heister, Katja
    Siewert, Christian
    Knicker, Heike
    [J]. ORGANIC GEOCHEMISTRY, 2009, 40 (03) : 332 - 342
  • [20] JONES TP, 1997, NATO ASI SERIES I, V51, P9