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Cerâmica

Print version ISSN 0366-6913

Cerâmica vol.56 no.338 São Paulo Apr./June 2010

http://dx.doi.org/10.1590/S0366-69132010000200010 

Synthesis of coloured ceramic pigments by using chromite and manganese ores mixtures

 

Síntese de pigmentos cerâmicos coloridos usando misturas de cromita e de minérios de manganês

 

 

M. H. AlyI; I. S. IsmaelII; F. BondioliIII

IEnvironmental Studies and Research Institute, Minufiya University, Sadat City, Minufiya, Egypt
IIGeological Department, Faculty of Science Suez, Suez Canal University
IIIDepartment of Material and Environmental Engineering, University of Modena and Reggio Emilia 41100 Modena, Italy

 

 


ABSTRACT

The aim of this work is not only the synthesis of black ceramic pigment with spinel structure using local and inexpensive minerals (chromite and manganese ores) but also throw some light on the relations between the structure and the colour of obtained pigment. Ultimate utilization spinel solid solution in ceramic materials is mostly due to their structure characteristics, their thermal and chemical stability. In this study colour pigments were ned by calcinations at 1250 ºC starting from a mixture of chromite and manganese oxide. Different compositions were tested containing 30, 40 and 50 wt.% of manganese oxide (low and high content respectively). The phase composition and microstructure characterization of both raw material and obtained pigments were evaluated by X-ray diffraction, X-ray fluorescence, polarizing microscope and scanning electron microscope. Furthermore, the colour measurements of the obtained pigments and tiles were evaluated. Composition of all pigments reveal the spinel structure with Cr2FeO4; hematite was also recorded in the mixture of low manganese. The degree of lightness is relatively same in the pigments mixtures of both manganese types. However, tiles could be considered lightness compared with its pigments, especially of the high manganese type. The solid state calcinations reactions are indeed able to form intense brown pigments that can be used as a stain for industrial ceramic applications. The production of less expensive black ceramic pigments from low cost and less pure raw materials that can be utilized in Egypt to substitute for the imported pure oxides or salts is proved superior performance for producing painted pigments.

Keywords: pigments, chromite, manganese ore, spinel, ceramic industry.


RESUMO

O objetivo deste trabalho é não somente a síntese de pigmento cerâmico negro com estrutura espinélio usando minerais locais e de baixo custo (minérios de cromita e manganês) mas também pesquisar as relações entre a estrutura e a cor dos pigmentos obtidos. O porquê da utilização de soluções sólidas de espinélio em materiais cerâmicos é principalmente devido às características estruturais, estabilidades térmica e química. Neste estudo pigmentos coloridos foram obtidos por calcinação a 1250 ºC partindo-se de mistura de cromita e óxido de manganês. Foram testadas diferentes composições contendo 30, 40 e 50 peso% de óxido de manganês (alto e baixo teor, respectivamente). A composição de fases e a caracterização microestrutural da matéria-prima e dos pigmentos obtidos foram avaliadas por difração de raios X, fluorescência de raios X, microscópio óptico com luz polarizada e microscópio eletrônico de varredura. Além disso, foram determinadas as cores dos pigmentos obtidos e dos azulejos. A composição de todos os pigmentos mostra a estrutura espinélio com Cr2FeO4; hematita foi também detectada na mistura de baixo teor de manganês. O grau de brilho é relativamente o mesmo em todas as misturas de pigmentos com os dois conteúdos de manganês. Entretanto, os azulejos podem ser considerados brilhantes comparados com seus pigmentos, especialmente o de maior teor de manganês. As reações de calcinação em estado sólido são realmente capazes de formar um pigmento marrom intenso que pode ser usado em aplicações em cerâmica industrial. A produção de pigmentos cerâmicos negros a partir de matéria-prima de menor custo e menor teor de pureza, que podem ser utilizadas no Egito para substituir os óxidos e sais puros, mostrou desempenho melhor para a produção de pigmentos pintados.

Palavras-chave: pigmentos, cromita, minério de manganês, espinélio, indústria cerâmica.


 

 

INTRODUCTION

The term pigments is applied to black, white or colored organic or inorganic powders that are insoluble in the substrate in which they are incorporated and are not chemically and physically altered by it [1]. Pigments used in the production of traditional colored glazed and unglazed tile must show thermal and chemical stability at high temperatures (1200-1250 ºC). The first step, in pigment production, is the selection of raw materials which are mostly metallic oxides or salts of the desired metals with industrial chemical purity.

The most important brown and black pigments used in ceramic coatings are the iron chromite spinels generally synthesized from mixture of iron oxide (Fe2O3) and chromium oxide (Cr2O3) by calcinations above 1000 ºC [2, 3]. Some of the black spinel pigments contain also other elements such as cobalt, manganese, nickel or copper. The cobalt free iron-chromium pigments have been the focus of renewed interest in recent years because of the increase in the price of cobalt-bearing black pigments and its pollution problems [4]. It was suggested that preparation of (Fe,Cr)2O3 solid solution as black pigments [4].

They used both mechanical mixing of oxides and coprecipitation of hydroxides to prepare a homogeneous mixed that were successively calcined to obtain the black pigments. This pigments appeared to be composed of a solid solution of (Cr,Fe)2O3 type, with prevalence of Cr1.3Fe0.7O3. The synthesis of an iron-chromium ceramic pigments by using limonite and chromite mixtures was investigated [5]. They mentioned that the chromite and limonite mixtures can be used as raw materials to obtain colors from dark brown to light brown depending on the calcinations temperature and chromite or limonite content.

Between the brown and black pigments are also manganese - chromite spinels that are prepared by calcinations of manganese oxide (MnO) and chromium oxide (Cr2O3) above 1000 ºC. This study is concerned with the evaluation of Egyptian manganese and chromite ores for the production of black ceramic pigments in order to substitute the imported pure oxides or salts. Pigments are an important part of the ceramic industries and most of these pigments are produced from expensive pure oxides and salts. Ceramic companies in Egypt are importing the pigment raw materials and the preparation of low cost even if less pure raw materials could be very interesting to produce coµmercial colors.

Chromite (FeO∙Cr2O3) is an important mineral used in refractories and as a colouring agent in enamel [6-8]. Chromite is characterized by high thermal and chemical stability compared with other minerals oxides, and can be used as inexpensive natural raw material to produce pigments. It is also reported that chromite addition to coµmercial black pigments reduced the cost of colouring glaze [9]. However, when raw chromite is used as colouring agent in glaze, brown spots may be produced and colour changes from yellow to brown depending on glaze composition.

Manganese oxides ore (MnO) can widely be found in the earth crust; MnO is a strategic oxide that has several industrial applications such as in steel production, carbon-zinc batteries production, fertilizers, as well as colorants for bricks, dyes and medicines [10]. The mineral coµmonly founded is pyrolusite that is sometimes added to red earths to create darker red, violet or black colors in pottery clays or glazes.

The aim of this work is not only the synthesis of black ceramic pigment with spinel structure using local and inexpensive minerals (chromite and manganese ores) but also throw some light on the relations between the structure and the colour of obtained pigment.

Sampling localities

Two manganese ore samples (high and low manganese content) were selected from Um Bogma area, situated in west central Sinai, 20 km east of the Gulf of Suez and 30 km south east of Abu Zenima (Fig. 1). Manganese deposits of Um Bogma form lenses in dolomitic and sandy beds at the based of Carboniferous sequence. The ore lenses are 1 to 200 m in diameter and up to 6 m thick [11, 12]. Chromite sample is selected from Abu Dahr area at about 3 km southeast of Bir Bitan (Fig. 1). Chromite occurs mainly as lenticular bodies of variable dimensions generally less than 10 m, coµmonly hosted by serpentinites [13].

 

 

EXPERIMENTAL PROCEDURE

Chromite and manganese oxide mixtures containing 30, 40 and 50wt.% of manganese oxide (low and high content respectively) were prepared. The mixtures were wet milled for three hrs in a ball mill and then dried. Each mixture was calcined for three hrs at 1250 ºC. The calcined product was wet grounded for 1h in a ball mill, washed, filtered and then dried.

After drying, the powders were tested as pigments for ceramic body coloring. A ceramic body, having a typical composition for gres porcellanato was used for pigment application. The pigments, added to the composition at 3wt.%, were dry mixed for 30 min. The mixtures were pressed at 400 kg/m2 and then fired at 1250 ºC for 40 min following an industrial cycle.

The chemical composition of raw materials were determined using Philips PW1410 X-ray fluorescence (XRF) at 50 kV and 40 mA. The mineralogical composition of raw materials and the crystalline phases obtained after calcinations were determined using Philips PW 1710 X-ray diffractometer (XRD), using Cu radiation (Kα=1.5418 Å) at 40 kV and 20 mA and Ni filter, with a scanning speed of two theta degree per minute. Colour measurements were performed using a colorimeter (Minolta CR 300) based on the CIE (Coµmission Internationale del'Eclarirage) system and the results were expressed as Hunter L* a* b* values. The colour measurements were carried out on pigments and colored tiles. Petrography of the natural raw materials were studied using Zeiss polarizing microscope, while grain and aggregate size of the obtained pigments were identified by SEM analysis using a Philips XL 30.

 

RESULTS AND DISCUSSION

The chemical composition of natural chromite, low and high manganese ores are listed in Table I.

 

 

Table I clearly shows that the chromite sample has Cr2O3 content of about 62.34% and Fe2O3 content of about 23.50%. On the other hand, high manganese ore sample has MnO content of about 78.83% and Fe2O3 content of about 13.41%, while in the low manganese ore sample the ratio between these two oxides is almost reversed (MnO 20wt.%; Fe2O3 71.5wt.%). SiO2 is relatively the same in all samples, while chromite demonstrated enriched in Al2O3 compared with manganese ores.

The X-ray diffraction patterns of nature raw materials are show in Fig. 2. From this figure it clear to note that, chromite ore is mainly contain chromite and small amount of antigorite and trace amount of chlorite, while low manganese ore is mainly composed of hematite with small amount of pyrolusite. On the contrary, high manganese ore is mainly composed of pyrolusite and small amount of hematite.

 

 

Reflected-light microscopy investigation shows that chromite is the main mineral in the chromite ore with grayish and low reflectivity grains, usually cracked and filled with serpentinites (Figs. 3a and 3b). Manganese ore shows, in good agreement with XRD results, that pyrolusite is the main Mn-oxides mineral present. Hematite is coµmon within Mn-oxide grains, particularly at the contact of cracked planes (Fig. 3c). Pyrolusite, alternative with hematite and goethite, forming zones, in some case hematite and goethite are filled voids between pyrolusite crystals (Fig. 3d).

Absence of manganese phases lines from X-ray diffraction patterns, may be reveals presence manganese as amorphous phase.

The X-ray patterns of obtained pigments are reported in (Fig. 4). The figure shows that at 1250 ºC, the spinel structure "Cr2FeO4" is formed independently from the starting raw materials even if hematite is also recorded in the mixture obtained starting from low manganese ore. Absence of manganese phases lines from X-ray diffraction patterns, may be reveals presence manganese as amorphous phase.

 

 

SEM analysis of pigments shows that they are mainly composed of a spherical or subspherical grains, its size ranges from 75-100 µm, the individual grain shows a concentrically band structure, these bands are alternative with each other (Figs. 5a and 5b).

 


 

Colour measurements

The measured values (Fig. 6) indicate that the degree of lightness of pigments, in relation to the scale that extends from white (L* =100) to black (L* = 0), is not influenced by the change of manganese content using low or high type. However L* values change considerably in tiles increasing the manganese content. In particular tiles are generally lightness compared with pigments, especially those with high manganese type.

 

 

Hunter b* values, in relation to the scale extending from blue (-b*) to yellow (+b*), are also not influenced by the manganese ore used. Finally the a* values in relation to the scale extending from green (-a*) to red (+a*), increase with increasing low manganese ore in pigments due to the higher content of red free hematite.

 

CONCLUSION

Local Egyptian chromite and manganese ores can be used as inexpensive raw materials to obtained colours pigments. Two manganese ore samples (high and low manganese content) were selected from Um Bogma area, situated in west central Sinai, and the other chromite sample is selected from Abu Dahr area. The colour pigments were prepared by the calcinations of chromite and manganese oxide mixtures containing 30, 40 and 50 wt% of manganese oxide (low and high content respectively) were prepared. In particular the mixtures during that calcination at 1250 ºC form a spinel structure of Cr2FeO4 type independently on the composition and mineral used. The colours of pigment range from dark black to light grey depending on chromite or manganese content. Pigments structure has a spherical or subspherical grains, with grain size ranging from 75 to 100 µm.

 

REFERENCES

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[2] A. Escardino, S. Mestre, A. Barba, V. Beltran, A. Blasco, Synthesis Mechanism of an Iron-Chromium Ceramic Pigment , J. Am. Ceram. Soc. 83, 1 (2000) 29-32.         [ Links ]

[3] A. Escardino, S. Mestre, A. Barba, V. Beltran, A. Blasco, Kinetic Study of Black Fe2O3-Cr2O3 Pigment Synthesis: I, Influence of Synthesis Time and Temperature, J. Am. Ceram. Soc. 86, 6 (2003) 945-950.         [ Links ]

[4] T. Manfredini, F. Bondioli, M. Romagnoli, Preparation of (Fe,Cr)2O3 solid solution as black pigment, Int. Ceram. J. (2000).         [ Links ]

[5] E. Ozel, I. Kucuk, S. Turan, Synthesis of an Iron-Chromium ceramic pigment by using Limonite and Chromite mixtures, Eng. Mater. 206-213 (2002) 187-1830.         [ Links ]

[6] S. H. Murdock, R. A. Eppler, Zinc Iron Chromite Pigments, J. Am. Ceram. Soc. 71, 4 (1988) C212-214.         [ Links ]

[7] R. I. Lazau, C. Pacurariu, D. Becherescu, R. Ianos, Ceramic pigments with chromium content from leather wastes, J. Eur. Ceram. Soc. 27, 2 (2007) 1899-1903.         [ Links ]

[8] E. Ozel, G. Unluturk, S. Turan, Production of brown pigments for porcelain insulator applications, J. Eur. Ceram. Soc. 26, 4 (2006) 735-740.         [ Links ]

[9] E. Ozel, S. Turan, Production and characterisation of iron-chromium pigments and their interactions with transparent glazes, J. Eur. Ceram. Soc. 23, 12 (2003) 2097-2104.         [ Links ]

[10] R. N. Sahoo, R. K. Srinivasa, Sulphating-roasting of low-grade manganese ore: optimization by factorial design, Int. J. Miner. Process. 25, 1-2 (1989) 147-152        [ Links ]

[11] A. M. Morsy, H. A. Hussein, A. M. El Fiky, Sedimentology of the Paleozoic in East Central Sinai. Proc. 3rd Conf. Geol., Ismailia (1992) 113-126.         [ Links ]

[12] G. S. Roufaiel, N. N. Yanni, K. M. Amer, Contribution to the study of manganese-iron deposits at Um Bogma area, Sinai. M.E.R. Ain Shams Univ., Earth Sci. 1 (1987) 98-107.         [ Links ]

[13] L. S. Ismael, Mineralogy and petrology of some chromite ores in the Eastern Desert, Egypt, B.Sc. Thesis, Faculty of Science, Ain Shams Univ., Cairo (1990) 84pp.         [ Links ]

 

 

(Rec. 15/05/2009, Ac. 01/03/2010)

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