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This article in SSSAJ

  1. Vol. 75 No. 3, p. 1125-1132
    Received: July 12, 2011

    * Corresponding author(s): David.Pare@nrcan.gc.ca


Black Spruce Soils Accumulate More Uncomplexed Organic Matter than Aspen Soils

  1. Jérôme Laganièreabc,
  2. Denis A. Angersd,
  3. David Paré *a,
  4. Yves Bergeronbc and
  5. Han Y. H. Chene
  1. a Natural Resources Canada Canadian Forest Service Laurentian Forestry Centre 1055 du P.E.P.S. P.O. Box 10380 Stn. Sainte-Foy Québec, QC Canada G1V 4C7
    b Centre for Forest Research Univ. du Québec à Montréal P.O. Box 8888 Stn. Centre-ville Montréal, QC Canada H3C 3P8
    c Univ. du Québec en Abitibi-Témiscamingue 445 boulevard de l'Université Rouyn-Noranda, QC Canada J9X 4E5
    d Agriculture and Agri-Food Canada Soils and Crops Res. and Dev. Centre 2560 Hochelaga Blvd Québec, QC Canada G1V 2J3
    e Faculty of Forestry and the Forest Environ. Lakehead Univ. 955 Oliver Road Thunder Bay, ON Canada P7B 5E1


Improving knowledge on the dynamics and maintenance of the boreal soil's C pool is of particular importance in response to climate change concerns. We hypothesized that different forest types (black spruce, trembling aspen, and mixedwood) found on a similar site type differentially affect soil organic carbon (SOC) distribution among physical fractions. The surface mineral soil (0–15 cm) of 24 plots differing in forest composition was sampled in forested Hapludalfs of the Abitibi-James Bay region, Canada. The soil was first separated into three water-stable aggregate size fractions (>1000, 1000–250, and <250 μm) by wet sieving, followed by a density flotation (NaI: 1.7 g cm-3) and a dispersion (with glass beads) to isolate the free light fraction (LF), the intraaggregate particulate organic matter (iPOM) and the silt plus clay fraction (S&C). According to mixed linear models, whole SOC contents (in Mg C ha-1) decreased in the following order: black spruce (46.3) > mixedwood (41.9) > trembling aspen (34.7). While similar amounts of SOC (∼30 Mg C ha-1) were found in the S&C, more SOC was found in the less protected fractions (i.e., uncomplexed organic matter, UOM: LF and iPOM) under black spruce than under trembling aspen, the mixedwood being intermediate. This higher accumulation of UOM under black spruce suggests a slower C turnover that is probably induced by the low-quality C inputs and environmental constraints to decomposition found in these forests. These differences in the amounts of SOC stored within soil physical fractions might have strong repercussions on the SOC budget of the boreal forest of eastern Canada under climate change.

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Copyright © 2011. Copyright © by the Soil Science Society of America, Inc.