Intensity cultivation induced effects on soil organic carbon dynamic in the western cotton area of Burkina Faso

被引:14
作者
Ouattara, Badiori
Ouattara, Korodjouma
Serpantie, Georges
Mando, Abdoulay
Sedogo, Michel P.
Bationo, Andre
机构
[1] Inst Environm & Rech Agr, Ouagadougou 04, Burkina Faso
[2] IRD, Antananarivo, Madagascar
[3] Int Ctr Soil Fertil & Agr Dev, Div Afrique, Lome, Togo
[4] CIAT, Trop Soil Biol & Fertil Inst, Nairobi 30677, Kenya
关键词
cultivation intensity; fallow; savannah; soil fractions; soil organic carbon;
D O I
10.1007/s10705-006-9023-0
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The soil organic carbon (SOC) dynamic is a key element of soil fertility in savannah ecosystems that form the key agricultural lands in sub-Saharan Africa. In the western part of Burkina Faso, the land use is mostly linked to cotton-based cropping systems. Use of mechanization, pesticides, and herbicides has induced modifications of the traditional shifting cultivation and increased the need for sustainable soil fertility management. The SOC dynamic was assessed based on a large typology of land cultivation intensity at Bondoukui. Thus, 102 farm plots were sampled at a soil depth of 0-15 cm, considering field-fallow successions, the cultivation phase duration, tillage intensity, and soil texture. Physical fractionation of SOC was carried out by separating the following particle size classes: 2,000-200, 200-50, 50-20, and 0-20 mu m. The results exhibited an increase in SOC stock, and a lower depletion rate with increase in clay content. After a long-term fallow period, the land cultivation led to an annual loss of 31.5 g m(-2) (2%) of its organic carbon during the first 20 years. The different fractions of SOC content were affected by this depletion depending on cultivation intensity. The coarse SOC fraction (2,000-200 mu m) was the most depleted. The ploughing-in of organic matter (manure, crop residues) and the low frequency of the tillage system produced low soil carbon loss compared with annual ploughing. Human-induced disturbances (wildfire, overgrazing, fuel wood collection, decreasing fallow duration, increasing crop duration) in savannah land did not permit the SOC levels to reach those of the shifting cultivation system.
引用
收藏
页码:331 / 339
页数:9
相关论文
共 47 条
  • [11] Soil organic carbon sequestration in tropical areas.: General considerations and analysis of some edaphic determinants for Lesser Antilles soils
    Feller, C
    Albrecht, A
    Blanchart, E
    Cabidoche, YM
    Chevallier, T
    Hartmann, C
    Eschenbrenner, V
    Larré-Larrouy, MC
    Ndandou, JF
    [J]. NUTRIENT CYCLING IN AGROECOSYSTEMS, 2001, 61 (1-2) : 19 - 31
  • [12] Feller C., 1991, Cahiers ORSTOM, Serie Pedologie, V26, P25
  • [13] Feller C., 1993, Soil organic matter dynamics and the sustainability of tropical agriculture: proceedings of an International Symposium, Leuven, Belgium, 4-6 November 1991., P77
  • [14] Feller C., 1983, Cahiers ORSTOM, Pedologie, V20, P223
  • [15] Carbon sequestration in clay mineral fractions from 14C-labeled plant residues
    Gonzalez, JM
    Laird, DA
    [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2003, 67 (06) : 1715 - 1720
  • [16] Jaiyeoba I. A., 1988, MALAYSIAN J TROPICAL, V18, P10
  • [17] Assessment of soil fertility restoration under fallow in Nigerian savannah
    Jaiyeoba, IA
    [J]. SOIL USE AND MANAGEMENT, 1997, 13 (03) : 163 - 164
  • [18] Lal R, 2000, ADV SOIL SCI-SER, P157
  • [19] Mathieu C., 1998, Analyse physique des sols. Methodes choisies.
  • [20] Mikha MM, 2004, SOIL SCI SOC AM J, V68, P809, DOI 10.2136/sssaj2004.0809