The pedogenesis of Planosolic soils, especially of the semi-arid “Agreste” region of Pernambuco State, Brazil, has n ot been properly studied. There are indications and doubts with regard to some aspects such as possible duality or differentiated reworked parent material, total of gains and losses and the relative mobility of the main constituent elements during soil evolution. Three soils with strong texture contrast were studied in a toposequence of the region. Three soils with a strong textural contrast on a […]