Nebkha dunes as indicators of wind erosion and land degradation in the Sahel zone of Burkina Faso

Nebkha dunes, which develop by the trapping of sand within the body of a plant, were investigated in the Sahelian zone of Burkina Faso. The characteristics, location and age of nebkhas were analysed in order to assess their significance as indicators of wind erosion and land degradation. Extensive field work was conducted during the dry seasons of 1991 and 1993. The positions in the terrain of the field observations were determined by satellite-aided ground navigation technology (GPS). Multi-temporal studies of changes in vegetation cover at the different nebkha sites were carried out by comparing aerial photographs and a SPOT image from different years. It was established that the nebkhas were formed by basically aeolian processes. Their occurrence was associated with areas having degraded vegetation and with human activities. Nebkhas were thus found to be good indicators of wind erosion and land degradation.

[1]  R. Folk,et al.  Brazos River bar [Texas]; a study in the significance of grain size parameters , 1957 .

[2]  Kenneth Pye,et al.  Aeolian sand and sand dunes , 1990 .

[3]  R. Bagnold,et al.  The Physics of Blown Sand and Desert Dunes , 1941 .

[4]  I. Reid,et al.  Desert Sediments: Ancient and Modern , 1988 .

[5]  A. Gunatilaka,et al.  Continental sabkha pans and associated nebkhas in southern Kuwait, Arabian Gulf , 1987, Geological Society, London, Special Publications.

[6]  N. Middleton Effect of drought on dust production in the Sahel , 1985, Nature.

[7]  S. Nicholson LONG‐TERM CHANGES IN AFRICAN RAINFALL , 1989 .

[8]  P. Hesp A review of biological and geomorphological processes involved in the initiation and development of incipient foredunes , 1989 .

[9]  L. H. Gile Coppice Dunes and the Rotura Soil1 , 1966 .

[10]  N. P. Woodruff,et al.  A Wind Erosion Equation , 1965 .

[11]  Nasa,et al.  A survey of anthropogenic vegetation changes in West Africa during the last century — climatic implications , 1985 .

[12]  Patrick A. Hesp,et al.  The formation of shadow dunes , 1981 .

[13]  Dale A. Gillette,et al.  Threshold velocities for input of soil particles into the air by desert soils , 1980 .

[14]  T. Littmann Rainfall, Temperature and Dust Storm Anomalies in the African Sahel , 1991 .

[15]  A. T. Grove,et al.  Geomorphological Studies in Southern Africa , 1989 .

[16]  David Ebdon,et al.  Statistics in geography , 1986 .

[17]  M. Sivakumar,et al.  Agroclimatology of West Africa: Burkina Faso , 1987 .

[18]  M. P. Petrov Types de déserts de l'Asie centrale , 1962 .

[19]  Sven Lindqvist,et al.  New evidence of desertification from case studies in Northern Burkina Faso , 1993 .

[20]  G. G. Pohlman Soil Science Society of America Proceedings , 1948, Soil Science Society of America Journal.

[21]  R. Purdie Land Systems of the Simpson Desert Region , 1984 .

[22]  Jong-Seop Lee THE ROLE OF DESERT SHRUB SIZE AND SPACING ON WIND PROFILE PARAMETERS , 1991 .

[23]  B. Toutain Essais de régénération mécanique de quelques parcours sahéliens dégradés , 1977 .

[24]  J. Prospero,et al.  Atmospheric transport of soil dust from Africa to South America , 1981, Nature.

[25]  M. Hulme Rainfall changes in Africa: 1931–1960 to 1961–1990 , 1992 .