『Abstract
Soil carbon sequestration is a viable short-term option to mitigate
increased atmospheric CO2. In agriculture,
strategies to increase the soil carbon (C) sink include no-tillage,
cover crops, and improved crop rotation. The objective of this
study was to determine the influence of tillage systems on SOC
and total N, soil aggregation and aggregate associated C and N
in three soil types: Oxisol (Brazil), Vertisol (Argentina), and
Mollisol (USA). Long-term tillage experiments included tilled
(T) and no-till (NT) systems. A native grassland was included
for comparison in each site. Soil samples were taken at 0-5, 0-15,
and 15-30 cm depths. Water-stable aggregates (WSA) were separated
using a wet-sieving method. Total C and total N were determined
by dry combustion. A shift from native grassland to an agroecosystem
decreased microbial biomass, but this decrease was less pronounced
under NT. Cultivation reduced the mass of macroaggregates and
the concentration associated C and N; however among agroecosystems,
NT, regardless soil type, tended to be more similar to the native
grassland sites. Agroecosystems reduced TOC and total N stocks,
regardless of soil type, compared to the native grassland. This
effect followed: Mollisol>Oxisol>Vertisol, and was more pronounced
at the 0-5 cm soil depth than at deeper depths. This loss of C
and N was associated with the decrease in the mass of macroaggregates
and lower C and N concentrations of the aggregates. Macroaggregation
was related to TOC and microbial biomass in the Mollisol, suggesting
that the biological process of aggregate formation is the principal
mechanism of C protection in these soils. The relationship between
TOC and large macroaggregates showed lower values for the Oxisol
and Vertisol, indicating that in these soils TOC has a complementary
role in macroaggregation.
Keywords: Aggregates; Tillage; Native grassland; No-tillage; Mollisol;
Vertisol; Oxisol』
Abbreviations
Introduction
Materials and methods
Site description
Soil sampling
Aggregate-size distribution
Total C and N
Total microbial biomass
Statistical analysis
Results
Total C and N
Aggregate distribution
Concentrations of C and N in aggregate fractions
Microbial biomass
Relationships among total C, soil aggregation and microbial biomass
Discussion
Acknowledgments
References