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Comparison of the transpiration of two types of vegetation cover in Northern Benin : an insight into the impacts of land conversion
Kohomlan Gbenakpon Beranger Awessou  1@  , Christophe Peugeot  2, *@  , Sylvie Galle  3, *@  , Euloge Agbossou  4, *@  , J Seghieri  5, *@  
1 : Hydrosciences Montpellier  (HSM)
Institut de Recherche pour le Développement, Université Montpellier 2 - Sciences et Techniques, Université de Montpellier, Centre National de la Recherche Scientifique : UMR5569
Univ. Montpellier - Case MSE Place Eugène Bataillon 34095 MONTPELLIER CEDEX 5 -  France
2 : HydroSciences Montpellier  (HSM)
IRD, CNRS, UM1, UM2
3 : Institut des Géosciences de l'Environnement  (IGE)
Institut de Recherche pour le Développement, Institut Polytechnique de Grenoble - Grenoble Institute of Technology, Centre National de la Recherche Scientifique : UMR5001, Université Grenoble Alpes
UGA - IGE CS 40700, 38058 Grenoble Cedex 9 -  France
4 : Laboratoire Hydraulique et de. Maitrise de l'Eau, Faculté des Sciences Agronomiques, Université d'Abomey-Calavi, Cotonou  (LHME / FSA)
5 : IRD-HydroSciences, BP 64501, 34394 Montpellier Cedex 5, France
Université Abdou Moumouni
* : Auteur correspondant

Sudanese Africa population growth is average 3% per year resulting in a significant increase in cultivated areas at the expense of fallows and forests. This land cover change is not without affecting the exchange of energy and water between soil, vegetation and atmosphere. For centuries, Sudanese rural population have been practicing agroforestry dominated by shea (Vitellaria paradoxa) parklands. We asked to what extent this practice can buffer the impact of the deforestation on the recycling of the water and therefore on the hydrological cycle. This preliminary study concern the woody cover only. Specifically, we compared transpiration of Vitellaria paradoxa (shea) that dominates agroforestry systems and of Isoberlinia doka that dominates forest, as indicator of shea water needs, at the tree and cover scale. Sap flow density (SFD) was measured by the transient thermal dissipation method from which transpiration of the tree was deduced then extrapolated at the species covers scale. Over the three-year of the study period (2011-2013), daily tree transpiration of V. paradoxa increased from 4 to 27 l/day according to tree diameter (8 to 38 cm respectively), while that of I. doka trees (diameters: 20 to 38 cm respectively) varied from 10 to 93 l.day-1. Transpiration varied lowly between wet and dry seasons in both species, suggesting that water is not the limiting factor, except a sharp drop during the period of leaves renewal (February-March). Transpiration of the cover of V. paradoxa was very low (0.03±0.01mm/day), corresponding to 0.42 à 1.32 % of the atmospheric demand estimated by reference evapotranspiration Eto, and 1.15 % of the annual rainfall, while that of the I. doka cover was 1.02±0.42 mm/day, corresponding to 7 to 74% of the atmospheric demand Eto, and 39.32 % of the annual rainfall. Our results indicates that agroforestry systems contributes more weakly to local evapotranspiration than the forest therefore the conversion of forests to fallow or agroforestry parkland could change the hydrological cycle. Thus, natural vegetation restoration efforts should be encouraged through reforestation campaigns in degraded areas to avoid droughts, water scarcity and the threat to food security.


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