Eame J., Gérard Martine, Bilong P., Suh C. E. (2009). Behaviour of elements in soils developed from nephelinites at Mount Etinde (Cameroon) : Impact of hydrothermal versus weathering processes. Journal of African Earth Sciences, 54 (1-2), p. 37-45. ISSN 1464-343X.
Titre du document
Behaviour of elements in soils developed from nephelinites at Mount Etinde (Cameroon) : Impact of hydrothermal versus weathering processes
Journal of African Earth Sciences, 2009,
54 (1-2), p. 37-45 ISSN 1464-343X
The progressive weathering of 0.65 Ma nephelinites from Mount Etinde (South Western Cameroon) in a humid tropical setting has resulted in the formation of a 150 cm thick weathering crust. The soil profiles consist of three horizons: Ah/Bw/C. A major differentiation of the chemical and mineralogical parameters is related to the complexity of the saprolites, some of which were hydrothermally altered. Bulk geochemical and microgeochemical analyses were performed on selected minerals from the different horizons of two reference profiles, of which one (E-4) was developed from unaltered nephelinite (nephelinite(U)) while the other (BO1) formed from hydrothermally altered nephelinite (nephelinite(H)). The results show that the primary minerals (clinopyroxene, nepheline, leucite, hauyne, titanomagnetite, perovskite, apatite and sphene) experienced differential weathering rates with primary minerals rich in rare earth elements (titanomagnetite, perovskite, apatite and sphene) surviving in the saprolite and the Bw horizons. The weathering of the primary minerals is reflected in the leaching of alkaline and alkaline-earth elements, except for Ba and Rb in the hydrothermalised nephelinite soil. The order of mobility is influenced by hydrothermal processes: Na > K > Rb > Ca > Cs > Sr in nephelinite(U) soil. Na > K > Sr > Ca > Mg in nephelinite(H) soil; Rb/Sr and Sr/Mg can be used as indicators of the kinetic of the weathering on nephelinite(U) and on nephelinite(H). Barium enrichment is related to variable concentrations in the nephelinites, to the formation of crandallites and the leaching of surface horizons. The content of metallic elements is higher in nephelinite(H) soil than in the nephelinite(U) soil. Results show that hydrothermal alteration leads to an enrichment of light (La, Ce, Nd) and intermediate (Sm, Eu, Dy) rare earth elements. The enrichment in Cr and Pb in the surface horizons is discussed in relation to organic matter activity, the dissolution of magnetites, and the impact of hydrothermal processes as well as atmospheric pollution in the case of lead.
