160
DRESVYANNIKOV, KOLPAKOV
in [24]}. The relative error of the indirect potentio-
metric determinations did not exceed 1%. The total Fe
content in the solution was additionally monitored by
X-ray fluorescence analysis (VRA-20L installation,
Carl Zeiss). Also, samples of the initial Al and the
reaction products were analyzed by X-ray phase anal-
ysis (DRON-3M diffractometer, CoK radiation,
1.79021 ) and electron microscopy (REMMA-
202M installation). The diffraction patterns were
identified using the JCPDS file [25]. Prior to analysis,
some deposit samples were kept in aqueous alkali to
remove excess Al, washed with double-distilled water
to neutral reaction and then with ethanol, and vacuum-
dried at 60 C.
Also, the diffraction patterns were processed with
the MAUD software [26].
The particle-size distribution of Al and Fe was
determined with an Analysette C-22 laser analyzer.
The measurements were performed using monochro-
Fig. 5. Image of an -Fe crystallite, obtained by re-
construction from X-ray diffraction data using the
MAUD software.
matic radiation with
638 nm.
REFERENCES
matrix, which is confirmed by direct experiment and
is satisfactorily described by the suggested model.
The reduction of Fe(III) ions with Al microparticles
is accompanied by the growth of the dendritic Fe
deposit; the final product consists of hollow spherical
particles with subnuclei on the surface and in pores.
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A-999 Al foil (specific surface area 37.0 cm2 g ).
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glass vessel equipped with an electric stirrer; the
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gas and under conditions of natural aeration showed
that atmospheric oxygen did not noticeably affect the
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tion kinetics was monitored by potentiometric titration
of samples taken at regular intervals {Fe(II) with bi-
chromate and Fe(III) with a complexone, as described
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