Carbon and nitrogen stocks and organic matter light fraction in a Typic Quartzipsamment under agricultural use

Authors

  • Leidivan Almeida Frazão Centro de Energia Nuclear na Agricultura
  • Ingrid Kely da Silva Santana Embrapa Solos
  • David Vilas Boas de Campos Embrapa Solos
  • Brigitte Josefine Feigl Centro de Energia Nuclear na Agricultura
  • Carlos Clemente Cerri Centro de Energia Nuclear na Agricultura

DOI:

https://doi.org/10.1590/S1678-3921.pab2010.v45.4579

Keywords:

Cerrado, pasture, conventional tillage, no-tillage

Abstract

The objective of this work was to evaluate C and N stocks in the soil and their contents in the free light fraction (FLL) of the soil organic matter (MOS), in a Typic Quartzipsamment under different land-use in Cerrado. Five areas were selected for evaluation: native cerrado; two areas with soybean under conventional tillage; one area formerly under pasture and afterwards cultivated with soybean under no-tillage; and one area under pasture with low productivity. Soil samples were collected from 0-5, 5-10, 10-20 and 20-30-cm depth layers to determine total C and N stocks of the soil. Contents of C and N in the FLL were determined at 0-5 and 5-10-cm depth. An increase was observed in the total C stocks in soybean areas implemented until five years, in comparison to the native cerrado area. There was a reduction in the amount of FLL and C content at 0-5 cm depth, in areas with soybean and pasture. Considering the low C and N natural input onto the Typic Quartzipsamment, the adoption of agricultural systems that can promote an adequate supply of residues is necessary for maintaining or increasing the soil organic matter.

Published

2011-01-27

How to Cite

Frazão, L. A., Santana, I. K. da S., Campos, D. V. B. de, Feigl, B. J., & Cerri, C. C. (2011). Carbon and nitrogen stocks and organic matter light fraction in a Typic Quartzipsamment under agricultural use. Pesquisa Agropecuaria Brasileira, 45(10), 1198–1204. https://doi.org/10.1590/S1678-3921.pab2010.v45.4579

Issue

Section

SOIL SCIENCE