Rb. Herbert et al., SURFACE-CHEMISTRY AND MORPHOLOGY OF POORLY CRYSTALLINE IRON SULFIDES PRECIPITATED IN MEDIA CONTAINING SULFATE-REDUCING BACTERIA, Chemical geology, 144(1-2), 1998, pp. 87-97
This study characterizes the surface chemistry and morphology of poorl
y crystalline iron sulfides precipitated in a chemically defined growt
h media for sulfate-reducing bacteria. The precipitates were analyzed
by X-ray diffractometry (XRD), X-ray photoelectron spectroscopy (XPS)
and scanning electron microscopy (SEM). Based on XRD results, the prec
ipitates exhibit only incipient crystallization with a single broad di
ffraction peak at about 5 Angstrom, characteristic of disordered macki
nawite. The iron sulfides generally exhibit a platy habit with particl
es 100 to 300 nm in diameter; these particles appear often in 1 to 2 m
u m spherical aggregates. The XPS results indicate that the Fe(2p(3/2)
) spectrum for poorly crystalline iron sulfide can be fitted with Fe(I
I) and Fe(III) components, both corresponding to Fe-S bond types, The
absence of oxide oxygen in the O(1s) spectrum and Fe(III)-O bond types
in the Fe(2p(3/2)) spectrum supports the conclusion that the poorly c
rystalline iron sulfides are composed of both ferric and ferrous iron
coordinated with monosulfide, with lesser amounts of disulfide and pol
ysulfides also present. These results suggest that the precipitates po
ssess a surface composition similar to greigite, with the remaining mi
neral mass composed of disordered mackinawite. (C) 1998 Elsevier Scien
ce B.V.