About Us | Help Videos | Contact Us | Subscriptions
 

Abstract

 

This article in JEQ

  1. Vol. 35 No. 4, p. 1599-1607
     
    Received: June 10, 2005


    * Corresponding author(s): tamado@smail.ufsm.br
 View
 Download
 Alerts
 Permissions
Request Permissions
 Share

doi:10.2134/jeq2005.0233

Potential of Carbon Accumulation in No-Till Soils with Intensive Use and Cover Crops in Southern Brazil

  1. Telmo Jorge Carneiro Amado *a,
  2. Cimélio Bayerb,
  3. Paulo Cesar Conceiçãob,
  4. Evandro Spagnolloc,
  5. Ben-Hur Costa de Camposd and
  6. Milton da Veigac
  1. a Department of Soil Science, Federal University of Santa Maria, Zip Code 97119-900, Santa Maria, RS, Brazil
    b Department of Soil Science, Federal University of Rio Grande do Sul, Zip Code 90001-970, Porto Alegre, RS, Brazil
    c Agricultural Research and Rural Extension Organization for the State of Santa Catarina (Epagri), Zip Code 88034-901, Florianópolis, SC, Brazil
    d Center of Experimentation and Research Fundacep, 98100-970, Cruz Alta, RS, Brazil

Abstract

The area under no-till (NT) in Brazil reached 22 million ha in 2004–2005, of which approximately 45% was located in the southern states. From the 1970s to the mid-1980s, this region was a source of carbon dioxide to the atmosphere due to decrease of soil carbon (C) stocks and high consumption of fuel by intensive tillage. Since then, NT has partially restored the soil C lost and reduced the consumption of fossil fuels. To assess the potential of C accumulation in NT soils, four long-term experiments (7–19 yr) in subtropical soils (Paleudult, Paleudalf, and Hapludox) varying in soil texture (87–760 g kg−1 of clay) in agroecologic southern Brazil zones (central region, northwest basaltic plateau in Rio Grande Sul, and west basaltic plateau in Santa Catarina) and with different cropping systems (soybean and maize) were investigated. The lability of soil organic matter (SOM) was calculated as the ratio of total organic carbon (TOC) to particulate organic carbon (POC), and the role of physical protection on stability of SOM was evaluated. In general, TOC and POC stocks in native grass correlated closely with clay content. Conversely, there was no clear effect of soil texture on C accumulation rates in NT soils, which ranged from 0.12 to 0.59 Mg ha−1 yr−1 The C accumulation was higher in NT than in conventional-till (CT) soils. The legume cover crops pigeon pea [Cajanus cajan (L.) Millsp] and velvet beans (Stizolobium cinereum Piper & Tracy) in NT maize cropping systems had the highest C accumulation rates (0.38–0.59 Mg ha−1 yr−1). The intensive cropping systems also were effective in increasing the C accumulation rates in NT soils (0.25–0.34 Mg ha−1 yr−1) when compared to the double-crop system used by farmers. These results stress the role of N fixation in improving the tropical and subtropical cropping systems. The physical protection of SOM within soil aggregates was an important mechanism of C accumulation in the sandy clay loam Paleudult under NT. The cropping system and NT effects on C stocks were attributed to an increase in the lability of SOM, as evidenced by the higher POC to TOC ratio, which is very important to C and energy flux through the soil.

  Please view the pdf by using the Full Text (PDF) link under 'View' to the left.

Copyright © 2006. American Society of Agronomy, Crop Science Society of America, Soil Science SocietyASA, CSSA, SSSA