Elucidation of the source and turnover of water soluble and microbial biomass carbon in agricultural soils

• Published in: Soil biology & biochemistry 2000-05, Vol.32 (5), p.581-587
• Main Authors: Gregorich, E.G., Liang, B.C., Drury, C.F., Mackenzie, A.F., McGill, W.B.
• Format: Article
• Language: English
• Subjects: 13C; Agronomy. Soil science and plant productions; Biological and medical sciences; Canada; Carbon dynamics; Chemical, physicochemical, biochemical and biological properties; Fundamental and applied biological sciences. Psychology; Maize; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Soil carbon; Soil microbial biomass; Soil science; Turnover; Water soluble organic carbon
• ISSN: 0038-0717; 1879-3428
• DOI: 10.1016/S0038-0717(99)00146-7

Understanding the dynamics of soil C is key to managing soil organic matter to enhance soil quality and ecosystem functioning, and reduce trace gas emissions from soils. Our objective was to determine the source and turnover of C pools in some agricultural soils in eastern Canada. Soils from five field experiments under continuous maize cropping for 4–37 yr were sampled, and the organic C content and stable C isotope ( 13C) composition of whole soil and water soluble and microbial biomass fractions determined. The 13C results showed a clear distinction between the water soluble organic C and microbial biomass C, with the water soluble organic C more like the whole soil and the microbial biomass more like the maize residues. A simple linear model was used to explore the relationship among the soil organic constituents and evaluate the turnover of these carbon pools. Even though the water soluble organic C had a higher turnover rate than the microbial biomass C, the proportion of C 4-derived C in the biomass was about 2.5 times greater than that in water soluble organic C. Apparently the large amount of native soil C, the small amount of water soluble organic C, and its equilibrium with the native soil C, cause humus to dominate the isotopic composition of water soluble organic C even though the water soluble C is very active. Our results suggest that the quantity, as well as the turnover rate, of soil organic matter constituents that are in equilibrium influence the isotopic composition of such constituents.