No tillage and crop rotation effects on soil aggregation and organic carbon in a Rhodic Ferralsol from southern Brazil

• Published in: Soil & tillage research 2005, Vol.80 (1), p.185-200
• Main Authors: Madari, Beáta, Machado, Pedro L.O.A., Torres, Eleno, de Andrade, Aluı́sio G., Valencia, Luis I.O.
• Format: Article
• Language: English
• Subjects: Agronomy. Soil science and plant productions; Biological and medical sciences; carbon; Carbon sequestration; Chemical, physicochemical, biochemical and biological properties; conventional tillage; crop rotation; Forest soil; forest soils; Fundamental and applied biological sciences. Psychology; genetic soil types; no-tillage; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Rhodic Ferralsols; Soil aggregate distribution; soil aggregates; soil aggregation; soil organic matter; Soil science; Subtropical climate; subtropical soils
• ISSN: 0167-1987; 1879-3444
• DOI: 10.1016/j.still.2004.03.006

In Brazil, no tillage (NT) is a soil conservation practice now widely adopted by farmers, including smallholders. The effect of NT and conventional tillage (disc ploughing followed by two light disc harrowings, CT) was investigated on the aggregation properties of a clayey Rhodic Ferralsol from southern Brazil under different crop rotations. The same soil type under secondary forest was used as reference. Macro- and microaggregate classes were separated by wet sieving using a series of eight sieves (8, 4, 2, 1, 0.5, 0.25, 0.125, 0.053 mm) at four sampling layers (0–5, 5–10, 10–20, 20–30 cm). The soil in general had high structural stability. At 0–5 cm, meanweight diameter (MWD, 11.1 mm) and total organic C in macroaggregates (TOC, 39 g kg −1 soil) were highest for the forest soil. Soil under NT had a more similar distribution of aggregate size classes and TOC to the forest soil than CT. The most pronounced difference between tillage systems was observed in the surface soil layer (0–5 cm). In this layer, NT had higher aggregate stability (AS NT: 96%; AS CT: 89%), had higher values of aggregate size distribution (MWD NT: 7.9 mm, MWD CT: 4.3 mm), and had on average 28% greater TOC in all aggregate size classes than CT. Soil under NT had greater TOC in macroaggregates (NT: 22 g kg −1; CT: 13 g kg −1). Crop rotation did not have a significant effect on soil aggregate distribution and TOC. By increasing macroaggregation NT increased organic carbon accumulation in soil.