Mobilization of Al and Ti during weathering — Isovolumetric geochemical evidence
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2013, Geochimica et Cosmochimica ActaCitation Excerpt :Consistent with such mobility, the Ti enrichments at depth observed in AL and PR can be attributed to the accumulation of Ti-bearing particles at depth rather than Zr mobility (Table 4) (Bern et al, 2011). Given these observations and other studies reporting higher Ti mobility compared to Zr in some lithologies (Gardner, 1980; Cornu et al., 1999; Neaman et al., 2006), Zr is the best choice of immobile element for this transect. Here, ρp and ρw are the bulk density of the parent (p) and weathered soil (w), respectively.
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