Organic matter storage in a sandy clay loam Acrisol affected by tillage and cropping systems in southern Brazil

Citation
C. Bayer et al., Organic matter storage in a sandy clay loam Acrisol affected by tillage and cropping systems in southern Brazil, SOIL TILL R, 54(1-2), 2000, pp. 101-109
Citations number
34
Categorie Soggetti
Agriculture/Agronomy
Journal title
SOIL & TILLAGE RESEARCH
ISSN journal
01671987 → ACNP
Volume
54
Issue
1-2
Year of publication
2000
Pages
101 - 109
Database
ISI
SICI code
0167-1987(200003)54:1-2<101:OMSIAS>2.0.ZU;2-R
Abstract
Soil organic matter decline and associated degradation of soil and environm ental conditions under conventional tillage in tropical and subtropical reg ions underline the need to develop sustainable soil management systems. Thi s study aimed first to evaluate the long-term effect (9 years) of two soil- tillage systems (conventional tillage: CT, and no-tillage: NT) and two crop ping systems (oat (Avena strigosa Schreb)/maize (Zea mays L.): O/M; and oat +common vetch (Vicia sativa L.)/ maize+cowpea (Vigna unguiculata (L.) Walp) : O+V/M+C without N fertilization on total organic carbon (TOC) and total n itrogen (TN) concentrations in a sandy clay loam Acrisol in southern Brazil . The second objective was to assess soil potential for acting as an atmosp heric CO2 sink. Under NT an increase of soil TOC and TN concentrations occu rred, in both cropping systems, when compared with CT. However, this increa se was restricted to soil surface layers and it was higher for O+V/M+C than for O/M, The O+V/M+C under NT, which probably results in the lowest soil o rganic matter losses (due to erosion and oxidation) and highest addition of crop residues, had 12 Mg ha(-1) more TOC and 0.9 Mg ha(-1) more TN in the 0-30.0 cm depth soil layer, compared with O/M under CT which exhibits highe st soil organic matter losses and lowest crop residue additions to the soil . These increments represent TOC and TN accumulation rates of 1.33 and 0.10 Mg ha(-1) per year, respectively. Compared with CT and O/M, this TOC incre ase under NT and O+V/M+C means a net carbon dioxide removal of about 44 Mg ha(-1) from the atmosphere in 9 years. NT can therefore be considered, as i t is in temperate climates, an important management strategy for increasing soil organic matter. In the tropicals and subtropicals, where climatic con ditions cause intense biological activity, in order to maintain or increase soil organic matter, improve soil quality and contribute to mitigation of CO2 emissions, NT should be associated with cropping systems resulting in h igh annual crop residue additions to soil surface. (C) 2000 Elsevier Scienc e B.V. All rights reserved.