Die Bindungsformen von Si,Mg, Fe,Al, Mn,Cr, Ni und Co in Saprolit und Laterit über Serpentinit,Insel Gebe,Indonesien

Fixation of Si, Mg, Fe, Al, Mn, Cr, Ni and Co in saprolite and laterite above serpentinite - Gebe Island, Indonesia The fixation of various major and trace elements has been studied in a saprolite/laterite profile above serpentinized peridotite. Sequential extraction of < 63 μm fraction shows different types of element fixation in soil: adsorption on mineral surfaces (1), fixation to Mn-oxides (2), bonding to poorly and better crystallized Fe-oxides (3). In the laterite, most of the extractable Si-, Al-, Cr- and Ni-contents are bound to goethitic Fe-hydroxide. The saprolite has considerable amounts of secondary quartz which has been formed during ageing of amorphous silica modifications. Their precipitation is favoured by high Si adsorption capacity of poorly crystallized Fe-hydroxide. In saprolite and laterite Co is bound to Mn-oxides. It can readily be extracted from pure Mn-oxides. In contrast, the intimate association of Mn-oxides to goethite reduces the rate of easily extractable Mn and Co in middle and upper zones of the laterite.