The pressure effect on the kinetics of ilmenite reduction in hydrogen
Abstract
A new process for ilmenite upgrading in the pigment industry has been proposed. The
process involves reduction of ilmenite in hydrogen under pressure. Past research in this
field of ilmenite reduction under pressure reveals a lack of understanding of the rates
and mechanisms involved.
A twin reactor, symmetrical-beam pressurised thermogravimetric microbalance was
designed and commissioned by the author. The system enabled the kinetics of
hydrogen reduction of ilmenite to be studied at high gas flow rates, where gas transport
resistances were minimised. The application of the micro-balance to mass loss
determinations, coupled with microscopic examinations of quenched reduction
products, were used to determine the mechanisms of oxygen removal from ilmenite
between temperatures of 823 and 1173 K up to pressures of 10 atm and 13 atm at the
lower temperatures. Natural ilmenite was initially investigated in a packed bed
arrangement but changes in experimental strategies led to in-situ gravimetric
examinations of synthetic ilmenite discs. Polishing the discs prior to reduction
eliminated the problem reported in an earlier study (Brigss and Sacco, 1991) of
nucleation and growth of iron metal over the surface of the discs to form a barrier to the
gas.
The reaction in a hydrogen atmosphere in the experimental conditions used had a
significant contribution from crystallographic control with parallel bands of
polycrystalline iron metal forming within the ilmenite grains of varying orientation.
The bands were parallel to the (0 0 0 1) basal plane of the parent ilmenite. Conversion
of ilmenite to rutile, Ti02, in the inter-band regions was also found to be
crystallographically controlled, with the b-axis of the rutile parallel to the c-axis of the
ilmenite, and the c-axis of rutile parallel to one of the three equivalent [1 1 0 0 ]
ilmenite directions. The hexagonal structure of ilmenite implies three possible
orientations of the rutile, giving triply-twinned rutile in the reduction products. The
twinned rutile grew perpendicular to the iron bands, consistent with fast solid-state
diffusion of metal ions along the c-axis of rutile. Although the metallisation within the individual ilmenite grams was
crystallographically controlled and was in the form of bands, the overall macroscopic
reduction within the poly-granular ilmenite discs was of the shrinking core
topochemical type. A shrinking core reduction model, modified to account for the
partial pressure build-up of reactant and product gases within the sample and for the
growth of pore size during reduction, was capable of predicting conversion-time
relationships of ilmenite samples. The change in reduction kinetics with increase in
applied pressure of the reactant gas was strongly influenced by the adsorption of
product gas onto the product solid. This resulted in a sharp increase in reaction rates up
to approximately 3 - 4 atm followed by a slow rate increase with any further pressure
mcrease.
The results of the modelling confirmed that at the lowest pressure used, 1.2 atm, and at
temperatures up to 1 023 K, the reduction reaction was predominantly under chemical
reaction control, particularly in the early stages of conversion. However the microscopy
studies indicated that solid-state diffusion is contributing in parallel with the interface
reaction. Knudsen diffusion is the major contributor to pore diffusion at the low
pressures. At 1123 K and 1.2 atm, the reduction is under mixed control with the
interface reaction and molecular pore diffusion both contributing. As the pressure is
increased, in addition to adsorption effects, molecular pore diffusion increases its
contribution to the control in the reduction kinetics.
Description
Keywords
Citation
Collections
Source
Type
Book Title
Entity type
Access Statement
License Rights
DOI
Restricted until
2033-11-15
Downloads
File
Description
DeVries_ExperimentalRates
DeVries_PartialPressures
DeVries_Var_Pore_DIAM