Premium
Mineralization Potential and Temperature Sensitivity of Soil Organic Carbon under Different Land Uses in the Parkland Region of Alberta, Canada
Author(s) -
Arevalo Carmela B. M.,
Chang Scott X.,
Bhatti Jagtar S.,
Sidders Derek
Publication year - 2012
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/sssaj2011.0126
Subject(s) - mineralization (soil science) , total organic carbon , organic matter , soil carbon , environmental chemistry , soil water , soil organic matter , grassland , chemistry , environmental science , soil science , agronomy , organic chemistry , biology
The temperature sensitivity of soil organic C contained in different particle‐size fractions is important in the context of global climate change but to date has been poorly studied. We compared the effects of temperature (7, 14, and 21°C) on C mineralization rates in fractionated soils from four land use systems [agriculture, AG; plantation; grassland, GRA; and native aspen ( Populus tremuloides Michx.) stand, NAT] in the parkland region of Alberta, Canada, over a 370‐d laboratory incubation. Carbon was largely held in the fine (<53 μm) fraction (59%), followed by the medium (53–250 μm, 31%) and coarse (250–2000 μm, 10%) fractions. Across land uses and incubation temperatures, the amount of C mineralized from bulk soil over 370 d ranged between 2 and 9% of initial total organic carbon (C i ), with mineralization rates based on per unit of C i ranging from 0.4 to 5.8 × 10 −4 mg C mg −1 C i d −1 and mean residence times (MRTs) ranging from 15 to 65 yr. Of the total amount of C mineralized, 77, 14, and 9% came from the coarse, medium, and fine fractions, respectively. The temperature sensitivity ( Q 10 ) of organic C under NAT increased with decreasing particle size, while plantation‐ and GRA‐derived soil organic C showed significantly greater Q 10 in the medium and fine fractions only. We conclude that the mineralization potential and temperature sensitivity of soil organic C in the studied land use systems were controlled mainly by organic matter quality and physical protection provided through aggregation and adsorption.