“…However, there were marked irregularities in these patterns, partly reflecting differ ences in the Al/Fe ratio of the soil. Obeng (1970) found Fe-P as the dominant and Ga-P as the lowest IP form in pro files of highly weathered iron-pan soils. His findings re flected the fact that the deeply leached condition under which the soils have been developed has given rise to almost a com plete removal of bases, hence, the low Ca-P status of the soils, and obviously accumulation of resistant sesquioxide resulted in high Fe-P values.…”