Runoff evolution due to land-use change in a small Sahelian catchment

被引:21
作者
Amogu, O. [1 ,2 ]
Esteves, M. [1 ]
Vandervaere, J-P. [3 ]
Abdou, M. Malam [1 ,2 ,3 ,4 ]
Panthou, G. [3 ]
Rajot, J-L. [5 ,6 ]
Yero, K. Souley [1 ]
Boubkraoui, S. [1 ]
Lapetite, J. -M. [1 ]
Dessay, N. [7 ]
Zin, I. [8 ]
Bachir, A. [4 ]
Moussa, I. Bouzou [4 ]
Maiga, O. Faran [4 ]
Gautier, E. [9 ]
Mamadou, I. [4 ,5 ,6 ,7 ,8 ,9 ,10 ]
Descroix, L. [1 ,2 ,3 ,4 ,5 ,6 ,7 ,8 ,9 ,10 ,11 ]
机构
[1] UJF Grenoble 1, CNRS, UMR 5564, IRD,G INP,LTHE, F-38041 Grenoble 9, France
[2] Coyne & Bellier, Tractebel Engn France, F-92622 Gennevilliers, France
[3] UJF Grenoble 1, CNRS, UMR 5564, G INP,IRD,LTHE, F-38041 Grenoble 9, France
[4] Univ Abdou Moumouni, Dept Geog, Niamey, Niger
[5] Univ Paris Est, AgroParisTech, CNRS, UMR 7618,IRD,UPMC,INRA,ENS,BIOEMCO, F-94010 Creteil, France
[6] U Paris Diderot, LISA, UMR 7583, UPEC,CNR, F-94010 Creteil, France
[7] UM2, IRD, UAG, UR ESPACE DEV UMR 228, F-34093 Montpellier 5, France
[8] UJF Grenoble 1, CNRS, UMR 5564, G INP,IRD,LTHE, F-38041 Grenoble 9, France
[9] Univ Paris 12, Univ Paris 01, Univ Paris 08, CNRS,UMR 8591, F-92195 Meudon, France
[10] Univ Zinder, Dept Geog, FLSH, Zinder, Niger
[11] IRD, MNHN, UMR PALOC, F-75231 Paris 5, France
来源
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES | 2015年 / 60卷 / 01期
关键词
land-use changes; duration of flow; runoff coefficient; Sahel; crusted soils; CLIMATE-CHANGE; WATER EROSION; RIVER; NIGER; DESERTIFICATION; CLASSIFICATION; INFILTRATION; VARIABILITY; GENERATION; DISCHARGE;
D O I
10.1080/02626667.2014.885654
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Land-use changes have been significant these last decades in West Africa, particularly in the Sahel region; in this area, climatic and demographic factors have led to a rise in cropped areas in recent decades causing strong changes in the water cycle and in river regimes. This study compares the rainfall-runoff relationships for two periods (1991-1994 and 2004-2011) in two small and similar neighbouring Sahelian catchments (approx 0.1 km(2) each). This allows identification of the different hydrological consequences of land-use/land-cover change, particularly the fallow shortening and the consequent degradation of topsoil. The main land surface change is a 75% increase in crusted soil area. Runoff increased by more than 20% on average between the two periods while flood duration decreased by 50% on average. However, runoff values remained largely constant in the lower part of the northern basin due to a strong increase in in-channel infiltration. Editor D. Koutsoyiannis; Associate editor T. Wagener
引用
收藏
页码:78 / 95
页数:18
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