Effect of a legume cover crop (Mucuna pruriens var. utilis) on soil carbon in an Ultisol under maize cultivation in southern Benin

被引:40
作者
Barthès, B
Azontonde, A
Blanchart, E
Girardin, C
Villenave, C
Lesaint, S
Oliver, R
Feller, C
机构
[1] IRD CIRAD, Lab MOST, F-34394 Montpellier 5, France
[2] Lab Sci Sol Eaux & Environm, CENAP, Cotonou, Benin
[3] Ctr INRA INAPG, Lab BIOMCO, F-78850 Thiverval Grignon, France
[4] Univ Lyon 1, Unite Rech IBIS, IRD,Lab Ecol Microbienne, UMR 5557,CNRS, F-69622 Villeurbanne, France
基金
中国国家自然科学基金; 加拿大健康研究院;
关键词
soil organic carbon; legume cover crop; mucuna; C-13 natural abundance; Benin;
D O I
10.1079/SUM2004235
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Long term fallow is no longer possible in densely populated tropical areas, but legume cover crops can help maintain soil fertility. Our work aimed to study changes in soil carbon in a sandy loam Ultisol in Benin, which involved a 12-year experiment on three maize cropping systems under manual tillage: traditional no-input cultivation (T), mineral fertilized cultivation (NPK), and association with Mucuna pruriens (M). The origin of soil carbon was also determined through the natural abundance of soil and biomass C-13. In T, NPK and M changes in soil carbon at 0-40 cm were -0.2, +0.2 and +1.3 t C ha(-1) yr(-1), with residue carbon amounting to 3.5, 6.4 and 10.0 t C ha(-1) yr(-1), respectively. After 12 years of experimentation, carbon originating from maize in litter-plus-soil (0-40 cm) represented less than 4% of both total carbon and overall maize residue carbon. In contrast, carbon originating from mucuna in litter-plus-soil represented more than 50% of both total carbon and overall mucuna residue carbon in M, possibly due to accelerated mineralization of native soil carbon (priming effect) and slow mulch decomposition. Carbon originating from weeds in litter-plus-soil represented c. 10% of both total carbon and overall weed residue carbon in T and NPK. Thus mucuna mulch was very effective in promoting carbon sequestration in the soil studied.
引用
收藏
页码:231 / 239
页数:9
相关论文
共 36 条
[1]  
Akobundu I. O., 1980, Proceedings 1980 British Crop Protection Conference - Weeds., P377
[2]  
[Anonymous], SSSA SPECIAL PUBLICA, DOI DOI 10.2136/SSSASPECPUB58.CH6
[3]  
[Anonymous], 2001, Climate Change 2001:Impacts, Adaptation and Vulnerability
[4]  
Azontonde A., 1993, Cahiers ORSTOM, Serie Pedologie, V28, P217
[5]  
Azontonde A., 1998, Agric. Dev, V18, P55
[6]   NATURAL C-13 ABUNDANCE AS A TRACER FOR STUDIES OF SOIL ORGANIC-MATTER DYNAMICS [J].
BALESDENT, J ;
MARIOTTI, A ;
GUILLET, B .
SOIL BIOLOGY & BIOCHEMISTRY, 1987, 19 (01) :25-30
[7]   Field-scale run-off and erosion in relation to topsoil aggregate stability in three tropical regions (Benin, Cameroon, Mexico) [J].
Barthès, B ;
Azontonde, A ;
Boli, BZ ;
Prat, C ;
Roose, E .
EUROPEAN JOURNAL OF SOIL SCIENCE, 2000, 51 (03) :485-495
[8]   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
[9]   Direct emission of nitrous oxide from agricultural soils [J].
Bouwman, AF .
NUTRIENT CYCLING IN AGROECOSYSTEMS, 1996, 46 (01) :53-70
[10]   Soil organic carbon and 13C abundance as related to tillage, crop residue, and nitrogen fertilization under continuous corn management in Minnesota [J].
Clapp, CE ;
Allmaras, RR ;
Layese, MF ;
Linden, DR ;
Dowdy, RH .
SOIL & TILLAGE RESEARCH, 2000, 55 (3-4) :127-142