Abstract
In the supergene environment under tropical climates, the behaviour of gallium depends on the physico-chemical conditions which control the evolution stages of the residual mantle and this element is not necessarily linked to aluminum, as was formerly believed. Ga vs. Al correlation is positive in weathering profiles from West Cameroon developed on granodiorite, basalt and trachyte, which essentially result from the leaching of alkalis, alkali-earths and silicon. However, in the upper part of the profile on trachyte, which underwent later aluminization, no significant Ga vs. Al correlation was evidenced. In lateritic and bauxitic profiles from Eastern Brazilian Amazonia developed on basalt and siliciclastic sedimentary rocks, the dissociation between gallium and aluminum is clearly expressed by a negative or lack of Ga vs. Al correlation in the bauxitic horizons, resulting mainly from intense aluminization, as well as in the ferruginous horizons. In turn, Ga vs. Fe correlation is markedly positive in both cases. Thus, when dissolution of early formed Ga-containing gibbsite and kaolinite occurs, aluminum migrates and concentrates in well differentiated zones while gallium tends to be leached out of the profile or is retained by Fe-oxyhydroxides.
Published Version
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