ISSN 0020ꢀ1685, Inorganic Materials, 2011, Vol. 47, No. 8, pp. 864–868. © Pleiades Publishing, Ltd., 2011.
Original Russian Text © A.I. Chepurov, V.M. Sonin, A.A. Chepurov, E.I. Zhimulev, B.P. Tolochko, V.S. Eliseev, 2011, published in Neorganicheskie Materialy, 2011, Vol. 47,
No. 8, pp. 957–961.
Interaction of Diamond with Ultrafine Fe Powders
Prepared by Different Procedures
A. I. Chepurova, V. M. Sonina, A. A. Chepurova, E. I. Zhimuleva,
B. P. Tolochkob, and V. S. Eliseevc
a Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences,
pr. Akademika Koptyuga 3, Novosibirsk, 630090 Russia
b Institute of SolidꢀState Chemistry and Mechanochemistry, Siberian Branch, Russian Academy of Sciences,
ul. Kutateladze 18, Novosibirsk, 630128 Russia
c Budker Institute of Nuclear Physics, Siberian Branch, Russian Academy of Sciences,
pr. Akademika Lavrent’eva 11, Novosibirsk, 630090 Russia
eꢀmail: chepurov@uiggm.nsc.ru
Received November 9, 2010
Abstract—We have studied the interaction of synthetic diamond crystals with ultrafine Fe powders during
catalytic diamond gasification in a hydrogen atmosphere at 900°C. The Fe powders were prepared by three
procedures: reduction of Fe2O3 nanopowder; evaporation using an ELVꢀ6 electron accelerator, followed by
condensation; and reduction of ferric chloride. The surfaceꢀprocessed diamond crystals were examined by
electron microscopy. The results indicate that ultrafine powders produced by the first two procedures cause
predominantly lateral etching of diamond. The Fe particles prepared by the third procedure penetrate into
the bulk of diamond crystals and produce etch pits and “tunnels,” thereby markedly increasing the specific
surface area of the crystals.
DOI: 10.1134/S0020168511070077
INTRODUCTION
laterally (along their faces), whereas natural diamond is
etched along the normal to its faces, with the formation
of very rough surfaces. Such studies were carried out for
Thermochemical (nonabrasive) processing of synꢀ
thetic and natural diamond is a chemical process
because it relies on catalytic diamond gasification in a
hydrogen atmosphere [1]. This process involves four
steps:
(1) transfer of carbon atoms from diamond to the
surface layer of the metal catalyst,
metal particles ranging in size from 1 to 3 m.
µ
This work examines the interaction of diamond with
smaller Fe particles (100 nm or less in size) prepared by
different procedures with the aim of studying the etching
behavior of diamond in the course of hydrogenolysis.
(2) carbon diffusion in the bulk of the metal,
(3) vaporization of the carbon dissolved in the metal,
and
EXPERIMENTAL
(4) the removal of the gaseous carbonꢀcontaining
species from the reaction zone.
Experiments were carried out in flowing hydrogen in
a waterꢀcooled temperatureꢀcontrolled microchamber
equipped with an observation window. The process was
followed using an MBSꢀ9 optical microscope. Hydroꢀ
gen was produced by an SGSꢀ2 electrolytic generator
and was introduced into the microchamber at a flow
rate of 3 l/h. The temperature was measured by a W/Re
thermocouple. The investigation technique was similar
to that described elsewhere [6, 7].
Several techniques for diamond processing are based
on this process: marking (including engraving), cutting,
deep pattern etching, lapping, polishing, and brazing of
metallic contacts to diamond [2]. In the last case, a
microscopically rough diamond surface is needed [3].
There is solid experimental evidence that, when
powder catalysts are used, etching with transition metal
particles depends on the crystallographic orientation of
the face and the structure of the diamond crystals [4, 5].
We studied diamond crystals grown on (001)ꢀoriꢀ
This effect is particularly highlighted by comparison of ented seeds in the Fe–Ni–C system at 5.5 GPa and
synthetic and natural diamond crystals. This is caused 1500 using a splitꢀsphere multianvil highꢀpressure
°C
by the presence of defects, around which interaction apparatus and a procedure described earlier [8]. The
mainly occurs. Synthetic diamond crystals grown under crystals had octahedral habits with cube and trapezoheꢀ
stable conditions are more perfect than natural diaꢀ dron modifying facets and belonged to type Iba accordꢀ
mond. For this reason, they are etched for the most part ing to the physical classification.
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