Abstract

The study of soil resources of Mayo-Danay, located in the tropical zone of Cameroon, shows a diversity of soils characterized by specific properties. Indeed, this study area is generally a plain landscape whose average relative altitude (300 m). However, it indicates a vegetation of savanna type, very dominant. Hydrologically, Logone River, Maga Lake and tributary streams of the Mandara Mountains regularly flood the study area. The sharing of these parameters leads to soil’s genesis, which have a sandy texture for floodplain soils and a very dominant clay texture for lacustrine soils. Otherwise, the geochemistry of these soils shows SiO2 contents globally 70% in the different soils studied; Al2O3 contents are less than 10% in lacustrine soils and less than 5% in floodplain soils; while the major elements data of soils such as Fe2O3, CaO and MgO indicate relatively low contents (≤2%) on soils studied. In addition, the mineralogy index of alteration expresses a moderate alteration of these soils. Thus, the distribution of these major elements of soil reveals its susceptibility to zonation, which is a consequence of intrinsic and extrinsic parameters to formation and differentiation of soils of the study area.

Highlights

  • Due to its position on the globe, Sudano-Sahelian zone is located in Africa between 9° and 13° Northern latitude

  • The northern part of the study area, around Maga Lake, lacustrine soils are generally located on an altitude unit less than more or less to 310 m and develop on floodplains with drying slots observed on the surface (1 m depth on average)

  • IJAESE– An Open Access Journal (ISSN: 2320 – 3609) mainly consist of periodically flooded grasslands associated with savannah shrubs with trees

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Summary

Introduction

Due to its position on the globe, Sudano-Sahelian zone is located in Africa between 9° and 13° Northern latitude. Identified in eastern part of this region, these flood plains locally named "yaéré", extend over about 10.000 km and start once crossed the Yagoua-Limani dune whose altitude are obviously less than 400 m; they consist essentially of alluviums of various types on which a variety of soils develop (Brabant and Gavaud, 1985; Garba, 2000) The soils of this sector dominated by sandy and clay texture, that are consequence of the direct contribution of the mountain zones located to above 800 m and piedmonts (between 400 and 800 m). The risks of gully erosion and flooding are obvious (Mamadou, 2000; Morin, 2000; Raunet, 2003; Sighomnou, 2003; Milleville and Serpantie, 1994; Seignobos and Moukouri, 2000)

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