Fjölrit RALA - 15.06.2004, Side 81

Fjölrit RALA - 15.06.2004, Side 81
Such behaviour is associated with the presence of exchangeable aluminum which accumulates in the lower part of the profile (horizons BC2 and C). The differences in the values of the chemical parameters of the two profiles EUROl and EUR02 can also be related to differences in soil management; in fact the EUROl profile show a lower content of organic matter and CEC. The profile EUR02 has very high values of CEC that was not correlated to the presence of organic matter. The micromorphological analysis has shown the rare presence of clay coatings in the C horizons along with pumice having different degree of weathering. The chemical analysis obtained by SEM - EDS on the same sections has shown that the silicon has accumulated in the extemal parts of the pumice; such areas appeared optically isotropic to the OM while aluminum has a very different distribution from the silicon. In addition other element mapping of the pumice in the thin sections have shown in prevalence similar distribution of alkaline cations, indicative of moderate weathering (Fig.l). Mineralogical composition of the clays has shown the presence of halloysite (hydrated form) with a peak at 1 nm and meta-halloysite with a peak at 0.72 nm. In the clayey fraction zeolitic minerals (mainly analcime and philippsite) have also been observed, in the deepest horizons ( (BCl, BC2 e C1 of the EUR02 profile), while in the top soil zeolites clearly decrease(Ming et al., 1989). In the sand fraction biotite, leucite, sanidine have been observed along with minor content of phillipsite ed analcime. The presence of such mineral related with higher values of CEC in the EUR02 profxle results of particular interest, to understand the weathering of the zeolites mineral and their influence on the specific chemical characteristics of the volcanic soil in the Flegrei Fields district. References Ming D. W., and Mumpton F. A. (1989). Zeolites in Soils. In Minerals in Soil Environments (2nd Edition) - SSSA Book Series, no.l., Ed. J. B. Dixon e S.B. Weed., 873-911. 62
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