Distribution of black carbon in ponderosa pine forest floor and soils following the High Park wildfire

被引:45
|
作者
Boot, C. M. [1 ]
Haddix, M. [1 ]
Paustian, K. [1 ,2 ]
Cotrufo, M. F. [1 ,2 ]
机构
[1] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80523 USA
[2] Colorado State Univ, Dept Soil & Crop Sci, Ft Collins, CO 80523 USA
关键词
ORGANIC-MATTER; PYROGENIC CARBON; FIRE; OXIDATION; CHARCOAL; BIOMASS; MIGRATION; SEDIMENT;
D O I
10.5194/bg-12-3029-2015
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Biomass burning produces black carbon (BC), effectively transferring a fraction of the biomass C from an actively cycling pool to a passive C pool, which may be stored in the soil. Yet the timescales and mechanisms for incorporation of BC into the soil profile are not well understood. The High Park fire (HPF), which occurred in northwestern Colorado in the summer of 2012, provided an opportunity to study the effects of both fire severity and geomorphology on properties of carbon (C), nitrogen (N) and BC in the Cache La Poudre River drainage. We sampled montane ponderosa pine forest floor (litter plus O-horizon) and soils at 0-5 and 5-15 cm depth 4 months post-fire in order to examine the effects of slope and burn severity on % C, C stocks, % N and BC. We used the benzene polycarboxylic acid (BPCA) method for quantifying BC. With regard to slope, we found that steeper slopes had higher C: N than shallow slopes but that there was no difference in BPCA-C content or stocks. BC content was greatest in the forest floor at burned sites (19 g BPCA-C kg(-1) C), while BC stocks were greatest in the 5-15 cm subsurface soils (23 g BPCA-C m(-2)). At the time of sampling, unburned and burned soils had equivalent BC content, indicating none of the BC deposited on the land surface post-fire had been incorporated into either the 0-5 or 5-15 cm soil layers. The ratio of B6CA : total BPCAs, an index of the degree of aromatic C condensation, suggested that BC in the 5-15 cm soil layer may have been formed at higher temperatures or experienced selective degradation relative to the forest floor and 0-5 cm soils. Total BC soil stocks were relatively low compared to other fire-prone grassland and boreal forest systems, indicating most of the BC produced in this system is likely lost, either through erosion events, degradation or translocation to deeper soils. Future work examining mechanisms for BC losses from forest soils will be required for understanding the role BC plays in the global carbon cycle.
引用
收藏
页码:3029 / 3039
页数:11
相关论文
共 50 条
  • [21] Natural severity of water repellency in pine forest soils from NW Spain and influence of wildfire severity on its persistence
    Rodriguez-Alleres, M.
    Varela, M. E.
    Benito, E.
    GEODERMA, 2012, 191 : 125 - 131
  • [22] Soil erosion modelling of burned and mulched soils following a Mediterranean forest wildfire
    Gonzalez-Romero, Javier
    Zema, Demetrio Antonio
    Carra, Bruno Gianmarco
    Neris, Jonay
    Fajardo, Alvaro
    Plaza-Alvarez, Pedro Antonio
    Moya, Daniel
    Pena-Molina, Esther
    de Las Heras, Jorge
    Lucas-Borja, Manuel Esteban
    SOIL USE AND MANAGEMENT, 2023, 39 (02) : 881 - 899
  • [23] Forest structure and fuels dynamics following ponderosa pine restoration treatments, White Mountains, Arizona, USA
    Roccaforte, John P.
    Huffman, David W.
    Fule, Peter Z.
    Covington, W. Wallace
    Chancellor, W. Walker
    Stoddard, Michael T.
    Crouse, Joseph E.
    FOREST ECOLOGY AND MANAGEMENT, 2015, 337 : 174 - 185
  • [24] Short-term effects of wildfire on microbial biomass and abundance in black pine plantation soils in Turkey
    Kara, O.
    Bolat, I.
    ECOLOGICAL INDICATORS, 2009, 9 (06) : 1151 - 1155
  • [25] Distribution of black carbon and black nitrogen in physical soil fractions from soils seven years after an intense forest fire and their role as C sink
    Lopez-Martin, Maria
    Javier Gonzalez-Vila, Francisco
    Knicker, Heike
    SCIENCE OF THE TOTAL ENVIRONMENT, 2018, 637 : 1187 - 1196
  • [26] NITROGEN CAN LIMIT OVERSTORY TREE GROWTH FOLLOWING EXTREME STAND DENSITY INCREASE IN A PONDEROSA PINE FOREST
    Marshall, L. A.
    Falk, Donald A.
    McDowell, Nate G.
    TREE-RING RESEARCH, 2019, 75 (01) : 49 - 60
  • [27] Snag longevity and surface fuel accumulation following post-fire logging in a ponderosa pine dominated forest
    Ritchie, Martin W.
    Knapp, Eric E.
    Skinner, Carl N.
    FOREST ECOLOGY AND MANAGEMENT, 2013, 287 : 113 - 122
  • [28] Objective and perceived wildfire risk and its influence on private forest landowners' fuel reduction activities in Oregon's (USA) ponderosa pine ecoregion
    Fischer, A. Paige
    Kline, Jeffrey D.
    Ager, Alan A.
    Charnley, Susan
    Olsen, Keith A.
    INTERNATIONAL JOURNAL OF WILDLAND FIRE, 2014, 23 (01) : 143 - 153
  • [29] Topographic controls on black carbon accumulation in Alaskan black spruce forest soils: implications for organic matter dynamics
    Kane, E. S.
    Hockaday, W. C.
    Turetsky, M. R.
    Masiello, C. A.
    Valentine, D. W.
    Finney, B. P.
    Baldock, J. A.
    BIOGEOCHEMISTRY, 2010, 100 (1-3) : 39 - 56
  • [30] Topographic controls on black carbon accumulation in Alaskan black spruce forest soils: implications for organic matter dynamics
    E. S. Kane
    W. C. Hockaday
    M. R. Turetsky
    C. A. Masiello
    D. W. Valentine
    B. P. Finney
    J. A. Baldock
    Biogeochemistry, 2010, 100 : 39 - 56