This study is an evaluation of the water potential of the Ferlo fossil
valley in the Louga area in Senegal. It consisted in determining the volume of
water that could be mobilized at the level of a confluence point of the waters
according to the flow lines, where a dam would be placed to create a reservoir.
This volume of mobilizable water was compared to the average water consumption
of the area in order to evaluate its adequacy or not. To do this, a
delineation, physical characterization and mapping of the Ferlo watershed was
done using Google Earth, Global Mapper and Arc GIS softwares. A catchment area
of 28,754 sq·km was obtained with a perimeter of 976 km, an average slope of
0.52% and a hydraulic length of 336 km. Then the decennial runoff of the
watershed was calculated using the CIEH method, this flow is estimated at 1120
cm/s. On the basis of this flow, the annual volume of water that can be
mobilized was estimated at 11,089,758 cm per year with a solid deposits of 93
cm per year. The conclusions reached are that there is a lack of mobilizable
water resources in the area and that the entire fossil valley needs to be
rewatered to provide a sustainable alternative water source.
References
[1]
Diop, D. (2008) Access to Water and Agriculture in the Senegal River Valley. GESTES, 13 p. https://opendocs.ids.ac.uk/opendocs/handle/20.500.12413/10345
[2]
Adams, A. (2000) Senegal River: Flood Management and the Future of the Valley. 31 p. https://www.iied.org/sites/default/files/pdfs/migrate/X170IIED.pdf?
[3]
Ba, D. (1996) Contribution to the Management of Health Risks Associated with the Re-Opening of the Lower Senegal River Valley. 85 p.
http://www.secheresse.info/spip.php?article55449
[4]
IAGU (African Institute of Urban Management) (2000) Environmental Profile of the City of Louga. 84 p.
https://staging.unhabitat.org/downloads/docs/2873_2434_lougaprofil.pdf
[5]
Fall, A. (2014) The Senegalese Ferlo: A Geographical Approach to the Vulnerability of Sahelian Anthroposystems. 379 p. https://hal.science/tel-01622314/
[6]
Diallo, M.D., Mahamat Saleh, M., Diallo, A., Bassene, C., Ndiaye, O., Niang, K., Diop, A. and Guisse, A. (2016) Characterization of Phenophase Vulnerability of Five Sahelian Plant Species in the Northern Ferlo Zone, Senegal. 19 p.
https://revist.net/REVIST_27/REVIST_27_10.pdf
[7]
Nicholson, S.E. (2000) Land Surface Processes and Sahel Climate. Review of Geophysics, 38, 117-139. https://doi.org/10.1029/1999RG900014
[8]
Tappan, G.G., Sall, M., Wood, E.C. and Cushing, M. (2004) Ecoregions and Land Cover Trends in Senegal. Journal of Arid Environments, 59, 427-462.
https://doi.org/10.1016/j.jaridenv.2004.03.018
[9]
Hountondji, Y.-C.H. (2008) Environmental Dynamics in the Sahelian and Sudanian Zones of West Africa: Analysis of Changes and Assessment of Vegetation Cover Degradation. University of Liège, Liège, 153 p. (In French)
[10]
Sy, O. (2010) Cross-Border Transhumance as a Source of Conflict in Ferlo (Senegal). Mappemonde, 98, 3 p.
http://mappemonde-archive.mgm.fr/num26/articles/art10201.html
[11]
Saidi, M.E. (2013) Contribution of GIS Software to Watershed Morphometry: The Example of Arc GIS. 9 p. http://saidi.ma/saidi2013.pdf
[12]
FAO (Food and Agriculture Organization) (1996) Floods and Inflows; Manual for Estimating Decadal Floods and Annual Inflows for Small Ungauged Catchments in Sahelian and Dry Tropical Africa. FAO, Rome, 265 p.
[13]
Van Tuu, N., Lemoine, B. and Pouplard, J. (1981) Road Hydraulics. BCEOM, 341 p.
[14]
Albergel, J. and Lamagat, J.P. (1991) Upper Senegal River Valley Master Plan. ORSTOM, Dakar.
[15]
Puech, C. (1984) Methods and References for the Design and Analysis of Hydro-Agricultural Schemes. Volume 1: Hydrology of Small Dams.