A range of allophane samples (atomic Al/Si bulk ratios 1.1-1.9) from S
ilica Springs, New Zealand, has been characterized by X-ray photoelect
ron spectroscopy (XPS). Binding energies of Si 2s, Si 2p, Al 2p, O 1s,
C Is, and N Is electrons, together with the kinetic energies of Al KL
23L23 Auger electrons, at or near the surface of allophane aggregates,
have been derived. The values for Al, Si and O electrons are similar
to those for kaolinite but also to those for some framework silicates
(feldspars) having 4-coordinate Al. Values for N electrons suggest tha
t N occurs in organic structures. Comparison of XPS and bulk Al/Si rat
ios shows an enrichment of Al at or near the surface of allophane aggr
egates. The same is true for C and N. Extraction with citrate-dithioni
te-bicarbonate (CDB) reagent leaves the surfaces depleted in Al. The C
DB extracts have higher Al/Si ratios than the bulk allophanes. Similar
ly, CDB treatment reduces the degree of surface enrichment of C and N.
Small increases in the binding energies of Si electrons following CDB
treatment suggest partial dissolution of the bulk structure though a
concomitant removal of a separate phase or species cannot be ruled out
. The results may be accounted for in terms of the structure previousl
y suggested for the primary spherules of Silica Springs allophane (Chi
lds et al., 1990) though the composition of the spherules at or near t
he surface of the allophane aggregates is different from those of the
bulk.