Phase and Microstructural characterization of chromite ore and
manufacturing of sodium dichromateChapter 2 (Literature review)
Submitted by: Asif khan & Waleed Subhan(BS Physics
Students)Submitted To: Dr. Yaseen Iqbal DEPARTMENT OF PHYSICS
UNIVERSITY OF PESHAWAR
CHAPTER II LITRATURE REVIEW1.1Chromite ore:The chemical formula
of chromite ore is FeO.Cr2O3 with Cr/Fe ratio as 2:1.Chromite ores
are basically classified on the basis of Cr2O3 content and Cr to Fe
ratio. Naturally occurring chromite minerals tends to have a spinel
structure, which is characterized by the partial substitution of
Mg2+, Ca2+ or Mn2+ for Fe2+ and Al3+ or Fe3+ for Cr3+ with the
general formula (Fe2+, Mg2+, Ca2+)O.(Cr3+, Al3+,Fe3+)2O3 [1].
Highest-grade chromite have Cr/Fe ratio more than 2 containing
minimum of 46 to 48 wt% Cr2O3. Chemical and refractory-grade
chromite typically have Cr/Fe ratios ranging from 1.4 to 2.0.
Chemical-grade (high-iron) chromite contain large amounts of iron
often results in Cr/Fe ratios of close to 1, absolute amount of
contained chromium ranges from 40 to 46 wt % Cr203. Low-grade
chromite have low Cr/Fe ratios and contain relatively small amounts
of chromium. Refractory-grade chromite contain relatively large
quantities of Al203 (greater than 20 wt %) and have Cr203+ Al203
level more than 60 wt % [2].1.2Phase and microstructural analysis
of chromite ore: Knowledge about particle size and distribution is
essential for a wide variety of industrial processes. To recover
minerals in the mineral processing industry, an ore must be ground
to produce liberated grains within the size range defined. Mineral
recoveries from a concentrator can often be improved by utilizing
mineralogical studies that affect mineral beneficiation. In order
to improve metal recovery of economic minerals in beneficiation,
the necessary quantitative mineralogical data can be obtained by
developed image analyzer [3], cone beam X-ray microtomography
system has been used for the quantitative analysis of multiphase
minerals, including grain size distribution, interfacial area,
textural information [4]. The use of an image analyzer in mineral
processing involves analyzing unbroken ore pieces to predict how
the minerals might behave during grinding and processing, and
analyzing ground ores and concentrated products to determine how
the minerals respond to processing [3]. The first step in studying
the unbroken ore is to identify minerals and their quantitative
appraisal in the ore. The second and the most important step is
size analysis for establishing size distribution. Higher value of
Cr content increases the significance of ore, but due to the
presence of impurities in the form of silicates, oxides, hydroxides
which reduces the value of the ore. To analyze the impurities
present in chromite ore was collected from Prangghar (Mohmand
agency), Pakistan [5]. Table 1 shows the minerals of different
sorts present in chromite ores [6].
1.3Phase analysis:The XRD data for the sample showed mainly 3
major peaks as shown in Figure 1. The EDX analysis carried out were
in agreement with XRD for the major compound, but some impurity
phases were also detected [5]. The pattern was matched with
magnesio-chromite-ferroan ((Mg, Fe) (Cr, Al)2 O4) ICDD card #
09-0353.According to the ICDD card data the spinel under
investigation has a cubic structure and almost all the iron is in
form of Fe2+ [6] however, a slight difference between the d-values
of the first peak and that of the database was observed. The
difference could be attributed to the change in the geological
location of specimen used in ICDD database, as it has been reported
to be from Cribou Canada having the composition: Cr2O3= 55.51%,
Al2O3= 14.03%, Fe2O3= 3.79%, FeO= 11.35%, MgO= 14.83% and minor Si,
Ti, Ca and Mn related compounds.[7]
Figure 1. The XRD pattern of the Mohmand agency chromite, the
data has possible match with ICDD card # 09-0353.
1.4Microstructural analysis:MMI showed four different type of
grain morphologies marked with G, H, I & J showing a different
phase for each. Figures 3(b,d) and 3(a,c) show the metallurgical
microscopy images and SEIs of the same area respectively. MMI of
samples when compared with SEM/EDX analysis revealed that both G
and H represented the same phase. The difference in grain
morphology (grain G being more continuous than H) might be due to
over etching of one region with respect to other. EDX of grains I
and J showed them as impurities but of different sort, this could
also be seen in color contrast of SEIs Figure 2(a, b) as I was
darker and J had whitish touch. EDX analyses of each grain in
Figure 2(a, b) are given in Table 2. From XRD, but based on SEM/EDX
the impurities could be mainly attributed to silicates family with
one of them being uvarovite [5].
Table 2. EDX analyses in weight% of the G, H, I and J grains
shown in Figure
Figure 2 (a,c) and (b,d) showing the SEI and MMI of the same
regions respectively. EDX analysis suggested that the grains G and
H represent chromite ore and I represent silicate impuritiesThe
chemical analysis of chromite ore samples exploited from
Philippines obtained from Bluestar Yima Chrome Chemical Materials
PR China is shown in table 3. The sample was crushed and dry-sieved
to four particle-size fractions (0.0450.063, 0.0630.075,
0.0750.090, 0.0900.150 mm), and then dried overnight at 80 C. The
Cr2O3 and Fe2O3 content of each size is given in table 4. All
experiments were performed with the 0.0450.063 mm. The potassium
hydroxide used in this work is of analytical grade and commercial
pure oxygen is used in this experiment [8].
Table 3 The chemical composition of Philippine chromite ore (%,
wt).
Table 4 Cr2O3 and FeO content in different size of Philippine
chromite ore.
The mineralogical analysis result of the Philippine chromite ore
indicates that the sample mainly consists of (Fe, Mg)(Cr, Fe)2O4
(Fig 3). The morphology of chromite ore was investigated by
scanning electron microscopy (SEM). Several important features can
be observed. (1) The solid particles have a compact surface (Fig.
4) and (2) The main elements including Cr, Fe and Al are uniformly
distributed in the chromite ore (Fig. 5), suggesting that chromite
ore has homogeneous structure [8].
Figure 3. XRD patterns of Philippine chromite ore. Figure 4. SEM
of Philippine chromite ore. Figure 5. The elemental distribution
map of Figure 4 detected by EDS.
The South African chromite ore from the Transvaal region of the
Bushveld complex was used for the investigation. The physical and
chemical properties of the ore analyzed by various techniques are
given in Table 5. The X-ray diffraction (XRD) pattern and the
microstructure of chromite ore is shown in figure 6 and 7
respectively. The XRD pattern of the ore indicates that the
chromium is mostly present in the (Fe, Mg)(Cr, Al)2 O4 spinel
phase. The microstructure shows primarily grains of well-defined
chromite spinel (bright phase) and a small quantity of siliceous
gangue (dark gray phase) [9].
Table 5 The Physical and Chemical Properties of South African
Chromite Ores.
Figure 6. The XRD pattern of the South African chromite ore. The
intensities are in arbitrary units (AU).
Figure 7. The microstructure of the chromite ore. Light gray
phases are the chromite minerals whereas the dark gray phase is
siliceous gangue.
The five types of chromite ore samples obtained from the
run-of-mines, obtained from Bantli which belongs to Karaburhan in
Eskisehir, Turkey; Dereboyu, Kef, Lasir and Yunuskuyu which belong
to Guleman in Elazig, Turkey. Chemical analysis of these chromites
by XRF (X-ray fluorescence) is given in Table 6. Lump samples of
chromites were made thin and polished sections and then these
sections have been investigated for the texture of chromite and
gang minerals. The representative samples of chromite ores were
examined by XRD and the patterns are given in Figure 8, 9 10, 11
and 12 [10].
Table 6. XRF analysis of chromite ores used
Figure 8. XRD patterns of BANTLI chromite ore. (Ore type
consists of serpentinized olivines as the gang mineral).
Figure 9. XRD patterns of (DEREBOYU) chromite ore. (Ore type
consists of pyroxene mineral as the gang mineral)
Figure 10. XRD patterns of (KEF) chromite ore. (Ore type
consists of mainly unaltered olivine minerals)
Figure 11. XRD patterns of (LASIR) chromite ore.
Figure 12. XRD patterns of (YUNUSKUYU) chromite ore. (Chromite
ore has dominantly serpentinized olivine as gang mineral).
Samples of chromite ores from South Africa (SA-1), India
(ICO-1), and China (CCO-1) were used for experiments. The main
differences between the three types of ores are apparent from their
physical and chemical properties, summarized by comparing the
chemical analysis in Table 7 and the X-ray diffraction (XRD)
patterns shown in Figure 13. In the South African ore, the chromite
spinel is predominant and the silica content is less than 1 wt%. By
comparison, the Indian ore, in addition to chromite spinel, also
consists of the gibbsite and Fe-rich sesquioxide solid solutions,
with silica at less than 1 wt%. The Chinese chromite, on the other
hand, was found to have approximately 6 wt% SiO2 in the form of
pure SiO2 and forsterite (Mg2SiO4) phases. Neither of these two
phases are present in the Indian and South African ores. The
scanning electron microscopic examination of ores also revealed a
considerable variation in the chemical compositions of chromite
grains in the Chinese ore, as compared to the average compositional
variation among the grains of the South African and Indian chromite
spinels. The overall chemical analysis of chromite ores was carried
out using the X-ray fluorescence spectrometric technique after the
loss-on-ignition (LOI) measurements at 1298 K. When the Chinese and
South African ores were heated in air for LOI analysis, both
samples gained weight due to the oxidation of FeO to Fe2O3, whereas
a major weight loss was observed in the Indian ore due to the
release of water of crystallization during the thermal
decomposition of gibbsite to constituent oxides [11].
Table 7. Physical and Chemical Properties of South Africa
(SA-1), India (ICO-1), and China (CCO-1) Chromite Ores
Figure 13. The XRD patterns of the South Africa (SA-1), India
(ICO-1), and China (CCO-1) chromite ore samples.
1.5Manufacturing of Chromium compounds (Traditional
Process):Chromium compounds are of considerable importance to many
industries, but their manufacturing is a major source of pollution.
Chromate plants discharge large amounts of chromium-containing
residues, dusts, and waste gases [12]. In the traditional process,
three problems are highly distinguishable. The first is the
environmental pollution. During production of one ton of chromium
anhydride (CrO3) product, the chromate production plant has to
discharge approximately 2.5 to 3.0 tons of toxic
chromium-containing residues that are difficult to be detoxified
and comprehensively used because of their high content of
hexavalent chromium. Also, the produced calcium chromate (CaCrO4)
is highly toxic and carcinogenic. Furthermore, the discharge of
large amounts of chromium-containing gases and dusts creates
serious pollution. The second problem is the low conversion
efficiency of the main element chromium. Although the reaction
temperature may be as high as 1200 C, the conversion efficiency of
chromium is only 76%, which means that a considerable amount of
chromium is discharged into the residue. The third problem with
this process is the production of by-products that are not
valuable. The chromium-containing Glaubers salt (Na2SO4.10H2O) and
sodium bisulfate (NaHSO4) produced are of little use and constitute
a pollution source [13]. Consequently, the total atom utilization
efficiency of the traditional process is quite low [14].The major
compounds which are manufactured are the chromates and the
dichromate of sodium, potassium and chromic acid. The main step in
manufacturing chromium compounds involves the conversion of the
water insoluble ore (chromite) into a water soluble chromate.
Finely grounded chromite (FeOCr2O3) is intimately mixed with sodium
carbonate (Na2CO3) and crude calcium carbonate (as dolomite or
limestone). This mixture is conveyed to a rotating furnace to be
roasted at 1100 0C. The limestone and dolomite acts as a mechanical
separator, allowing oxygen to react with the chromite and sodium
carbonate (Na2CO3) A series of chemical reactions takes place which
can be represented as follows [15, 16].
1. 4 (FeOCr2O3) + 4 (Na2CO3) 4 (Na2Cr2O4) + 4 (FeO) + 4 (CO2)2.
4 (Na2Cr2O4) + 4 (Na2CO3) + 6 (O2) 8 (Na2CrO4) + 4 (CO2)3. 4 (FeO)
+ (O2) 2 (Fe2O3)
Calcium carbonate is added to increase heat of the reaction some
calcium chromate is formed during the process and is mostly
decomposed by excess soda. The red hot roasted product (frit) is
transferred to wash tanks where hot water is carefully added this
flooding give rise to a strong exothermic reaction, as a result
sodium mono chromate is leached out and the liquor run off and is
treated according to special treatments. In order to obtain
dichromate, the mono chromate liquor is treated with dilute
sulphuric acid (H2SO4) in special tanks. The reaction proceeds as
[15].
4. 2 Na2CrO4 + H2SO4 Na2SO4 + Na2Cr2O7 + H2OThe sodium sulphate
is less soluble then the dichromate and much of it separates out
and is removed more sodium sulphate separates and is removed. The
final mother liquor contains the dichromate which crystallizes out
on concentration. In order to obtain potassium dichromate a
concentrated solution of potassium salt (e.g potassium chloride) is
added to a concentrated solution of sodium dichromate. Potassium
dichromate is precipitated immediately. Another chromium compound
is chromic acid (CrO3) is prepared by adding strong sulphuric acid
to a concentrated solution of potassium dichromate, the reaction is
given as [15].
5. K2Cr2O7 + H2SO4 K2SO4 +H2O +2 CrO3Partial drying of the
principle products, namely potassium and sodium mono- and
dichromate is carried out in filter presses and the process
completed in centrifugal dryers or heated baths [15].Figure 14
represents the flow sheet of the traditional process used for
producing chromic oxide (Cr2O3) from chromite ore. The traditional
process does not extract all of the chromium from the chromite ore.
The residue contains unreacted chromite ore and un-extracted
chromate, and usually must be disposed of on-site. The chromium
containing sodium sulfate (Na2SO4) formed as a byproduct has little
commercial value and also must be disposed of on-site [16].
Figure 14. Illustrate flow sheet of traditional production
process for chromic oxide (Cr2O3)1.6Green manufacturing process of
chromium compounds:A green manufacturing process for chromium
compounds has been developed by the Institute of Process
Engineering, Chinese Academy of Sciences [17], with the design
objective of eliminating pollution [18] the green process includes
continuous oxidization of chromite ore in a sub molten salt medium
at 300 C coupling of reaction and separation, recovery, and
recycling of the reaction medium and comprehensive use of the
multiple components in chromite ore. The essence of the green
process is that traditional oxidation roasting of chromite ore with
sodium carbonate at 1200 C is replaced by continuous liquid-phase
oxidation of chromite ore in the sub molten salt medium at 300 C in
a multiphase reactor. at the source The new cleaner process is
based on the principles of cleaner production and industrial
ecology [19], and aims to achieve the 3Rs (Reduce, Recycle, Reuse)
objectives Combining environmental and economic benefits, the goals
of comprehensive use of resources, recycling of reaction media, and
zero emissions should be achieved in the green process. Figure 15
illustrates the main design idea of the proposed new green process,
according to the reactions (6,7,8,9,10) [16].
Figure 15. Schematic idea of the proposed green manufacturing
process for chromium compounds.1.6.1To Reduce: A new reaction path
(reaction 6, 7, 8) was designed and no solid additives were needed
in the oxidation of chromite ore, the amount of waste residue
remaining following leaching was remarkable reduced. The reactants
such as (CO2) (reaction 9) and carbon black (C) (reaction 10) we
employed to convert the semi-finished products to the final
products, minimizing possible pollution sources.[16]6. FeO.Cr2O3 +
2KOH + 7/8 O2 Fe2O3 + H2O + K2CrO47. MgO.Cr2O3 + 2 KOH + O2 MgO +
H2O + K2CrO48. Cr2O3 + 2 KOH + 3/4 O2 H2O + K2CrO49. 2 K2CrO4 + H2O
+ 2 CO2 K2Cr2O7 + 2 KHCO310. K2Cr2O7 + C Cr2O3 + K2CO3 + CO1.6.2To
Recycle:An excessive amount of potassium hydroxide (KOH), in
sub-molten salt state, was employed as the reaction medium, and
most was recycled after the reaction occurred. Only a small amount
was consumed during the reaction and needed to be supplemented
[16].
11. 2 KHCO3 K2CO3 + H2O + CO212. K2CO3 + Ca(OH)2 CaCO3 + 2
KOH13. CaCO3 CaO + CO214. CaO + H2O Ca(OH)21.6.3To Reuse:The
produced intermediates such as potassium carbonate (K2CO3) and
potassium bicarbonate (KHCO3) were reused to manufacture potassium
hydroxide (KOH) (reaction 11, 12) the calcium hydroxide (Ca (OH) 2)
can be recovered (reaction 13, 14) [20].In the new cleaner process,
illustrated in figure 16 aluminum-bearing by products and
magnesium-bearing byproducts are manufactured, in addition to the
products of potassium dichromate (KCr2O7) and chromic oxide (Cr2O3)
[21]. As the final obtained ferrite-enriched residues were used as
raw materials in the cement industry [16].
Figure 16. Illustrative ow sheet of the new cleaner production
process for chromic oxide (Cr2O3).
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