Unique role of pore water in lateritic bauxite formation, Republic of Guinea

M. Makarova, V. Mamedov, Y. V. Alekhin, E. Shipilova
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引用次数: 1

Abstract

Results of the hydrogeochemical study of bauxite-bearing lateritic mantles of the Futa Djallon-Mandingo Province, West Africa, have allowed us to first characterize the pore water of vadose and infiltration hydrogeological zone. Abundances of major components (aluminum and iron) of the water are shown to be few orders higher than are those typical of the other waters of lateritic mantles. The pore water is proved to be a major factor of matter redistribution over any bauxite-bearing lateritic profile.
孔隙水在几内亚红土铝土矿地层中的独特作用
通过对西非富塔贾隆-曼丁戈省含铝土矿红土地幔的水文地球化学研究,首次对渗透和渗透水文地质带的孔隙水进行了表征。水的主要成分(铝和铁)丰度显示比其他红土地幔水的典型丰度高几个数量级。孔隙水被证明是任何含铝土矿红土剖面上物质再分配的主要因素。
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