Controle de la solubilite du fer et de l'aluminium en milieu ferrallitique

Details Controle de la solubilite du fer et de l'aluminium en milieu ferrallitique Controle de la solubilite du fer et de l'aluminium en milieu ferrallitique

Jul 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982gecoa..46.1267s&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 46, Issue 7, pp.1267-1279

Physics

Scientific paper

The Fe and Al content of ground and surface waters of a toposequence sampled in Central Cameroun are interpreted as being controlled by equilibrium interactions of water and secondary mineral phases in the macroscopic system. Calculations based on the known thermodynamic properties of ferric hydroxide and kaolinite are consistent with this hypothesis, though microsystems making up the macrosystem contain ephemeral phases that are not in equilibrium with phreatic waters.

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