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Carbon Distribution in a Hummocky Landscape from Saskatchewan, Canada
Author(s) -
Landi A.,
Mermut A. R.,
Anderson D. W.
Publication year - 2004
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2004.1750
Subject(s) - pedogenesis , carbonate , geology , organic matter , total organic carbon , soil science , soil carbon , soil organic matter , grassland , loess , environmental science , mineralogy , soil water , geomorphology , environmental chemistry , chemistry , ecology , organic chemistry , biology
Changes in the topography influence organic and inorganic C contents and δ 13 C values of soil C across a landscape. The objectives of this research were to: (i) study the effect of landscape on the formation and distribution of pedogenic carbonate and organic matter distribution in a hummocky landscape, and (ii) estimate the amount of organic C and pedogenic carbonate accumulation in local scale in comparison with regional scale using the stable isotope geochemistry techniques and standard characterization analyses. A hummocky landscape, typical of 38% of Saskatchewan's land, with glacial till parent material under virgin grassland, was studied. Organic C content of A horizons range between 20 to 98 g kg −1 Both extremes occurred in level positions of the south‐facing and north‐facing slopes. The lowest δ 13 C value of organic C (−29.6‰) was measured in a depression and the highest (more positive) was obtained on a shoulder (−21.7‰). The δ 13 C values of carbonate ranged from −0.9‰ (carbonated parent material) at the 114‐cm depth in level complex to −7.9‰ at depth of 100 cm in footslope complex and depression. The amount and percentage of pedogenic carbonate was higher in north‐facing slopes than in southward slopes. The highest proportion and amount of pedogenic carbonate up to 1‐m depth was found in Calcicryolls in footslope complex position in the north‐facing slope, and likely represents a gain in carbonate through lateral flows. The lowest proportion and amount (34.4% and 33.9 kg m −2 ) was found in the shoulder complex segment of west‐facing slope and in footslope complex position in east‐west direction. On average, the rate of accumulation is about 1.25 g C m −2 yr −1 of inorganic C (pedogenic carbonate) and 1.25 g C m −2 yr −1 as organic C. These are close to the calculated rate of 1.4 g C m −2 yr −1 for Dark Brown, and 1.3 g C m −2 yr −1 for Black soils (Mollisols) in Saskatchewan.