Carbon storage in labile fractions of soil organic matter in a tropical no-tillage Oxisol

被引:122
作者
Bayer, C
Martin-Neto, L
Mielniczuk, J
Pavinato, A
机构
[1] Univ Fed Rio Grande Sul, Dep Solos, BR-90001970 Porto Alegre, RS, Brazil
[2] Embrapa Instrumentacao Agropecuaria, BR-13560970 Sao Carlos, SP, Brazil
[3] SLC Agricola, BR-98920000 Porto Alegre, RS, Brazil
关键词
tropical soils; greenhouse effect; conservative agriculture; soil management;
D O I
10.1590/S0100-204X2004000700009
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
Carbon storage in the soil organic matter (SOM) is an important strategy to mitigate carbon dioxide concentration in the atmosphere. The objective of this study was to evaluate the effect of the no-tillage (NT) use for six years, under four autumn (dry-season) cover crops based maize and soybean crop rotations (pigeon pea-pearl millet, bengan hemp-sorghum, sunflower-black oat, and wild radish-maize), on C storage in the particulate (>53 mum) and mineral-associated (<53 mum) SOM fractions of a clayey Oxisol from Brazilian Cerrado region. In comparison to conventional tillage (CT) under summer cash-crops, NT increased the total organic carbon (TOC) stocks in the surface soil layer (0-5 cm). In the top 20 cm layer, NT soil under wild radish-maize had 9% (4.66 Mg ha(-1)) more TOC than the conventionally tilled soil. On the other hand, C storage in NT soil under other cropping systems was statiscally similar to the CT soil. The C stocks in the particulate SOM fraction increased by 37 to 52% in NT soil (0-20 cm) in comparison to CT. The higher sensitivity to soil management changes made the particulate organic matter a more adequate soil quality index compared to the TOC stocks. The C stock in the mineral-associated SOM fraction was not affected by soil management systems, which can be related to the short-term under NT and or to the highly stable soil microaggregates in this clayey Oxisol. The preferential C storage in the labile SOM fraction is an environmental benefit, which is expected to occur only under continuous no-tillage and crop residues addition.
引用
收藏
页码:677 / 683
页数:7
相关论文
共 26 条
[1]  
[Anonymous], THESIS U FEDERAL DO
[2]  
*ASS PLANT DIR CER, 2004, PLANT DIR TROP
[3]   Relationship of soil organic matter dynamics to physical protection and tillage [J].
Balesdent, J ;
Chenu, C ;
Balabane, M .
SOIL & TILLAGE RESEARCH, 2000, 53 (3-4) :215-230
[4]   Stocks and humification degree of organic matter fractions as affected by no-tillage on a subtropical soil [J].
Bayer, C ;
Mielniczuk, J ;
Martin-Neto, L ;
Ernani, PR .
PLANT AND SOIL, 2002, 238 (01) :133-140
[5]   Changes in soil organic matter fractions under subtropical no-till cropping systems [J].
Bayer, C ;
Martin-Neto, L ;
Mielniczuk, J ;
Pillon, CN ;
Sangoi, L .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2001, 65 (05) :1473-1478
[6]  
Bayer C., 1999, FUNDAMENTOS MAT ORGA, P9
[7]   MORPHOLOGICAL CHARACTERIZATION OF SOIL CRUST DEVELOPMENT STAGES ON AN EXPERIMENTAL FIELD [J].
BRESSON, LM ;
BOIFFIN, J .
GEODERMA, 1990, 47 (3-4) :301-325
[8]   CARBON TURNOVER IN SOIL PHYSICAL FRACTIONS [J].
BUYANONOVSKY, GA ;
ASLAM, M ;
WAGNER, GH .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1994, 58 (04) :1167-1173
[9]   PARTICULATE SOIL ORGANIC-MATTER CHANGES ACROSS A GRASSLAND CULTIVATION SEQUENCE [J].
CAMBARDELLA, CA ;
ELLIOTT, ET .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1992, 56 (03) :777-783
[10]  
CASSOL EA, 1984, B TECNICO, V15