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Publication Details
AFRICAN RESEARCH NEXUS
SHINING A SPOTLIGHT ON AFRICAN RESEARCH
agricultural and biological sciences
Microbiology and macrofaunal activity in soil beneath shrub canopies during residue decomposition in agroecosystems of the sahel soil biology & biochemistry
Soil Science Society of America Journal, Volume 77, No. 2, Year 2013
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Description
A major limitation for crop productivity in degraded Sahelian soils is the lack of organic inputs. Piliostigma reticulatum (DC.) Hochst and Guiera senegalensis J. F. Gmel. are unrecognized and unmanaged shrubs of the Sahel that coexist with crops and have potential to provide significant amounts of organic inputs to improve soil quality. However, conventional management involves coppicing and burning aboveground biomass every spring before crop plantings. Therefore, the objective of this study was to develop fundamental microbial information about nonthermal decomposition of these residues as influenced by the shrub canopy, litter, and root system. An experiment was done for P. reticulatum or G. senegalensis that had a 2 by 3 by 2 factorial design with two soil treatments (beneath and outside the influence of the shrub), three residue amendments (leaf, stem, and leaf + stem), and two litterbag mesh size treatments (plus, >2 mm, or minus macrofauna). Litterbags were destructively sampled at 15, 30, 60, 120, and 210 d after the first rain. At each sampling, litter mass was determined, and the soil beneath the litter bag was assessed for microbial properties and inorganic N. The presence of macrofauna stimulated mass loss, microbial biomass carbon (MBC), enzyme activities, and inorganic N. Rates of decomposition and microbial response with soils beneath were higher than outside the canopy. The results provide a basis for developing improved, non-thermal management of coppiced shrub residue while still allowing preparation of favorable seedbeds for row crops. Previous research has shown that these shrubs can do hydraulic redistribution (HR) of water from wet subsoil to dry surface soil. The higher soil moisture beneath shrubs in our experiment indicates that HR is a contributing factor to drive decomposition and nutrient mineralization in the dry season. Copyright © 2013 by the Soil Science Society of America, Inc.
Authors & Co-Authors
Diedhiou-Sall, Sire
Senegal, Ziguinchor
University of Ziguinchor
Dossa, Ekwe L.
United States, Muscle Shoals
International Center for Soil Fertility and Agricultural Development
Diédhiou, Ibrahima
Senegal
Université de Thiès
Badiane, Aminata Niane
Senegal, Dakar
Ag/nrm
Assigbétsé, Komi Bruno
Senegal, Dakar
Institut de Recherche Pour le Développement Dakar
Samba, Samba Arona Ndiaye
Senegal
Université de Thiès
Khouma, Mamadou
Senegal, Dakar
Institut Sénégalais de Recherches Agricoles Dakar
Séné, Modou
Senegal, Thies
Ceraas
Dick, Richard Patrick
United States, Columbus
The Ohio State University
Statistics
Citations: 39
Authors: 9
Affiliations: 8
Identifiers
Doi:
10.2136/sssaj2012.0284
ISSN:
03615995
e-ISSN:
14350661
Research Areas
Environmental
Study Approach
Quantitative