Storage and forms of organic carbon in a no-tillage under cover crops system on clayey Oxisol in dryland rice production (Cerrados, Brazil)

被引:42
|
作者
Metay, Aurelie
Moreira, Jose Aloisio Alves
Bernoux, Martial
Boyer, Thomas
Douzet, Jean-Marie
Feigl, Brigitte
Feller, Christian
Maraux, Florent
Oliver, Robert
Scopel, Eric
机构
[1] ISTOM, Coll Adv Studies Int Agrodev, F-95094 Cergy Pontoise, France
[2] EMBRAPA CNPAF, BR-75375000 Santo Antonio de Goias, Go, Brazil
[3] IRD, UR041, Lab MOST, F-34394 Montpellier 5, France
[4] CIRAD TA, F-34398 Montpellier 5, France
[5] Univ Sao Paulo, CENA, BR-13400970 Piracicaba, SP, Brazil
[6] CIRAD, I-00100 Rome, Italy
[7] EMBRAPA, BR-73301970 Planaltina, DF, Brazil
来源
SOIL & TILLAGE RESEARCH | 2007年 / 94卷 / 01期
关键词
oxisol; no-tillage; carbon sequestration; particle-size fractionation of SOM; Cerrados; Brazil;
D O I
10.1016/j.still.2006.07.009
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The management and enhancement of soil organic carbon (SOC) is very important for agriculture (fertility) as well as for the environment (carbon (C) sequestration). Consequently, changes in soil management may alter SOC content. No-tillage (NT) practices are potential ways to increase SOC. We studied the SOC from agricultural soils in the Cerrados in Central Brazil. We compared two different tillage systems: conservation agriculture with no-tillage under cover crops (NT) and disc tillage (DT) for 5 years in a context of rainfed rice production. The soil is a dark red Oxisol with high clay content (about 40%). The objectives of the study were: (i) to evaluate the short-term (5 years) impact of tillage systems on SOC stocks in an Oxisol and (ii) to better understand the dynamics of SOC in different fractions of this soil. We first studied the initial situation in 1998, and compared it to the 2003 situation. NT with cover crop (Crotalaria) was found to increase the storage of C in the topsoil layer (0-10 cm) compared to DT. The difference observed for the 0-10 cm layer under NT in comparison with DT represented C enrichment under no-tillage amounting to 0.35 Mg C ha(-1) year(-1) and corresponding to less than 10% of cover crops residues returned to the soil. A particle-size fractionation of soil organic matter (SOM) showed that differences in total SOC between NT and DT mainly affected the 0-2 mu m fraction and, to a smaller extent the 2-20 mu m fraction. This specific enrichment of SOC in the silt and clay fraction was attributed to (i) the storage of a water soluble C in the field and (ii) the effect of soil biota and especially fauna activity. The mean residence time of carbon associated with the fine fractions being rather long, it might be assumed that the preferential storage in fine fractions resulted in a long-term carbon storage. This study suggests a positive short-term effect of a no-tillage system on C sequestration in an Oxisol. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:122 / 132
页数:11
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