The paper describes the analysis of a columbite-tantalite (coltan) mineral ore from
Congo by using total reflection X-ray fluorescence (TRXRF) analysis. The sample was
mineralised with a lithium tetraborate and lithium metaborate flux mixture. TRXRF allows
multi-element analysis in a wide range of concentrations. The results were in good
agreement with those obtained by using another alkaline fusion with sodium peroxide

Ceccon L

Ciraolo L

Lo Coco F

Novelli V

Valentini C

English

Lo Coco, Filippo

Novelli, Veronica

Ceccon, Luciano

Ciraolo, L

Valentini, C.

Institutional Research Information System

Characterisation of Columbite-Tantalite (Coltan) ore from Congo. Elemental composition by total reflection X-ray fluorescence analysis

LO COCO, Filippo

NOVELLI, Veronica

CECCON, Luciano

Valentini C.

Archivio istituzionale della ricerca - Università degli Studi di Udine

CHARACTERISATION OF COLUMBITE-TANTALITE (COLTAN) ORE FROM CONGO. ELEMENTAL COMPOSITION BY TOTAL REFLECTION X-RAY FLUORESCENCE ANALYSIS Filippo Lo Coco∗, Veronica Novelli∗∗, Luciano Ceccon∗, Luigi Ciraolo∗∗∗, Clemente Valentini∗∗∗∗∗Department of Economic Sciences. University of Udine, Via Tomadini 30/A, Udine,filippo.lococo@dse.uniud.it luciano.ceccon@dse.uniud.it∗∗Department of Chemical Sciences and Technologies, University of Udine, Via Cotonificio 108, Udine, v.novelli@dstc.uniud.it∗∗∗Department of Studies on Resources, Enterprise, Environment and Quantitative Methodologies, University of Messina, Piazza S. Pugliatti 1, Messina, luigi.ciraolo@unime.it∗∗∗∗Chemical Laboratory of Customs of Turin, Corso Sebastopoli 3, Turin, lab1torino@finanze.itAbstract The paper describes the analysis of a columbite-tantalite (coltan) mineral ore from Congo by using total reflection X-ray fluorescence (TRXRF) analysis. The sample was mineralised with lithium tetraborate and lithium metaborate flux mixture. TRXRF allows multi-element analysis in a wide range of concentrations. The results were in good agreement with those obtained using another alkaline fusion with sodium peroxide.  Keywords: TRXRF; Alkaline Fusion; Elemental Composition; Columbite-Tantalite;1. Introduction Columbite-tantalite ore is known as Coltan in some African countries. It is occur mainly as an accessory mineral disseminated in granitic rocks or in pegmatites associated with granites where columbium (niobium, Nb, is the actual name) and tantalum are present in the form of mixed oxides corresponding to the general formula (Fe,Mn)(Ta,Nb)2O6 (1) with widely varying ratios of Nb to Ta. When niobium predominates over tantalum the mineral is known as columbite; when the reverse is true the proper name is tantalite. Coltan ore exist in all continents but most deposits with relatively high niobium or tantalum content are small and erratically distributed. Most of the niobium and tantalum metal produced todays extracted from columbite-tantalite ore is obtained from Africa, Brazil, Australia and India. For niobium alone, pyrochlore and bariochlore is another important source mineral found in countries like Canada, Brazil and Norway (2-5). Niobium as ferroniobium is used extensively in the steel industry as an additive in the manufacture of high strength, low alloy and carbon steels. Niobium and many of its alloys exibit superconductivity, thus they are of great interest for propulsion devices, electronic devices and other applications. Tantalum is used in chemical industry equipment for reaction vessels and heat exchangers in corrosive environments. In 1994 over 72% of the tantalum produced in yhe world went into the manufacturing of solid tantalum capacitors atti di euroconference on university and enterprise2for use in the most demanding electronic applications. The very low corrosion rate and inertness of tantalum make it attractive for many biomedical applications (2). The elemental composition of mineral ores is of great importance in the classification and grading of the ores. Qualitative and quantitative data on ore samples are of great interest to mineral prospectors and investors because it is very important to be sure of the quality/grade of the ores they are dealing with. There is, therefore, a need for a multi-elemental analytical technique for the analysis of the solid mineral samples. Usually inductively coupled plasma atomic emission spectrometry (ICP-AES) or atomic absorption spectrometry (AAS), energy dispersive X-ray fluorescence (EDXRF) spectrometry and total reflection X-ray fluorescence (TRXRF) spectrometry were used (6-9). In this paper we have employed a TRXRF technique in the analysis of a sample of coltan from Congo, previous an alkaline fusion with lithium tetraborate and lithium metaborate flux mixture. The results were compared with those obtained with another alkaline fusion utilizing sodium peroxide (10-11). 2. Experimental 2.1. Standards and Reagents All glassware was rinsed with 5% (v/v) pure nitric acid (C. Erba, Milan, Italy). High- quality water (18.2 MΩ) obtained from a Milli-Q water purification system (Millipore, Milford, MA, USA) was used exclusively. Ultra-pure and certified hydrofluoric acid (C. Erba), pure lithium tetraborate (BDH, Poole, UK), pure lithium metaborate (BDH), pure sodium peroxide (BDH), scandium (III) standard solution containing 1,000 mg L-1 of scandium (J. T. Baker, Deventer, The Netherlands) and gallium (II) standard solution containing 1,000 mg L-1 of gallium (J. T. Baker) were used. 2.2. Instrumentation and Software TRXRF analysis was performed on TX2000 spectrometer (Ital Structures, Riva del Garda, Italy) that consists of a x-ray tube with an alloy anode of Molybdenum/tungsten, a monochromator of the X-ray beam that use a highly reflective multilayer made of Si/W , a solid state lithium-drifted silicon detector Si(Li) that is cooled with liquid nitrogen (resolution energy range 135 eV to 5.9 keV and 1000 cps). The equipment runs under TXRFACQ32 program that includes facilities for data acquisition, spectrum analysis and interpretation and quantitative analysis. Both Mo-tube and W-tube excitation were used for analysis with tube setting of 40 kV and 20 mA. Live time was 600 s. 2.3. Analytical Procedure 2.3.1. Preliminary Sample Processing A coltan ore sample was ground finely on a vibratory disc mill. A 0.15-g coltan ore sample so obtained was fused with 10 g of lithium tetraborate and lithium metaborate mixture (1:3, w/w) in a platinum crucible and kept in the muffle furnace for half hour at 900 °C. The cooled melt was dissolved adding 90 mL of ultrapure water acidified with 4 % (v/v) hydrofluoric and 6% (v/v) nitric acid. atti di euroconference on university and enterprise3Another aliquot of 0.12-g was fused with 1.2 g of sodium peroxide in a graphite crucible and kept in the muffle furnace for half hour at 550 °C. The cooled melt was treated first with 90 mL of ultrapure water at 80 °C for 15 min and then with 1 mL of hydrofluoric acid and 4 mL of nitric acid heating until obtaining a clear solution. 2.3.2. Determination of elemental composition A 10-µL of the sample solution obtained in the preceding section was transferred on to quartz sample carrier. 1 mL of scandium (III) solution as internal standard and 1 mL of gallium (II) solution to control the matrix effect wer added. The sample was evaporated at 100 °C and the analysis were carried out with Mo- Kα  and W-Lα. The conversion of the signals in concentrations occurs by operations of fitting in order to minimise the deviations between the fit/background and the spectrum. 3. Results and Discussion Multi-element analysis by total reflection X-ray fluorescence spectrometry has evolved during two decades. At the present there are commercial equipments available for the chemical analysis in all kind of biological and mineral samples. The technique of analysis in TRXRF is founded on the same principles of conventional X-ray fluorescence measurements. When radiation passes from a medium of lower density to one of higher density it is totally reflected if the angle of incidence is below a certain critical angle, tipically a few milliradians of X-ray. By illuminating the sample with a beam that is being totally reflected, the absorption of the beam in the supporting substrate is largely avoided and the associated scattering is greatly reduced. So the background noise is reduced. A further contribution to the reduction of background noise is obtained by minimising the thickness of the sample; minimal quantity of sample (10-100 µL) is required for the analysis, the solvent is evaporated and a thin film a few nanometers thick remains and the matrix effect is eliminated. In this work TRXRF analysis was used for the qualitative and quantitative determination of most elements in a coltan mineral ore. In Figure 1 a TRXRF spectrum of the mineral ore was reported and as may be seen accurate multi-element analysis was obtained.  Figure 1. TRXRF Mo-Kα spectrum of a coltan sample from Congo. Scandium (III) wasadded as internal standard. For conditions of analysis see Experimental. atti di euroconference on university and enterprise4To estimate the matrix effect a solution of gallium (II) was added at the sample obtaining a recovery ranging from 95% to 110%. Quantitative analysis was carried out utilising scandium (III) as internal standard because of its lack in the sample. The results obtained are reported in table 1. Table 1. Elemental composition of a coltan mineral ore. MAJORS % w/w SD RSD% LOD % SOURCE Nb 24 2 7 0,3 W-La Ta 11,7 0,6 5 0,015 Mo-Ka Fe 8,2 0,4 5 0,01 Mo-Ka Mn 5,4 0,4 8 0,015 Mo-Ka Sn 3,39 0,04 1 0,06 W-La W 1,18 0,09 8 0,015 Mo-Ka Ti 1,12 0,06 6 0,015 W-La TRACES PPM SD RSD% LOD (PPM) SOURCE Ca 4705 256 5 300 W-La V <200 200 Mo-Ka Cr <200 200 Mo-Ka Se <30 30 Mo-Ka Y 1071 72 7 20 Mo-Ka K <500 500 Mo-Ka Rb <20 20 Mo-Ka Sr 152 40 26 20 Mo-Ka Pb 488 147 30 70 Mo-Ka Th 221 87 39 40 Mo-Ka U 1094 126 12 40 Mo-Ka Ce 968 196 20 280 W-La Nd 608 23 4 250 W-La The table 1 reportes major elements in percent in weight and trace metals in mg kg-1(ppm). All data are the results of two independent measurements and relative standard deviation is less than 8% for major elements. Table 1 relate also the detection limits (LOD) calculated by the following equation LOD = 3 C (Ipeak)-1 square root Iback were C, Ipeak, Iback represent the amount of the element, net intensity (cps) of the peak of the element and background intensity (cps) respectively (12). Table 2 compares the obtained results analysing  the samples with two distinct alcaline fusions. The correlation parameters between the two alcaline fusions are given  by  the  straight  line  (reported in Figure 2) equation Y = 0.99487 (± 0.01984) + 197.2 (± 1239.3) (n = 14). A paired t-test showed that no significant differences exist between the two alkaline fusions. atti di euroconference on university and enterprise5Figure1. Straight line obtained plotting results analysing a coltan mineral ore with two distinct alkaline fusion. Table 2. Elemental composition (mg Kg-1) of a coltan mineral ore analysed with two distinct alcaline fusion. Element LiBO2/Li2B4O7 Na2O2Ti 11093 10765 V 200 200 Cr 200 200 Mn 61221 52282 Fe 83874 79772 Y 1117 1007 Nb 174558 173569 Ta 112179 119155 Sn 24615 27099 W 7151 12545 Sr 129 189 Pb 308 539 Th 215 138 U 1269 979 4. Conclusion The TRXRF technique was employed in the analysis of a columbite-tantalite mineral ore. Due to its multi-element capability and high sensitivity TRXRF is a valuable tool for elemental composition of mineral ores. 0500001000001500002000000 50000 100000 150000 200000LiBO2/Li2B4O7 - ppmNa2O2 - ppmatti di euroconference on university and enterprise6Acknowledgment The Authors thank Dr. Amedeo Cinosi of Sasol SpA for technical support. References     1)  H.H. Read, Rutleys Elements of Mineralogy, George Allen & Unwin, London, 1976. 2) Kirk-Othmer Encyclopedia of Chemical Technology (4th ed.) New York, Wiley, 1997. 3) R.L. Parker, J.W. Adams, Niobium and Tantalum, U.S. Mineral Resources, U.S. Geological Survey Professional Paper 820, 1973, 443. 4) Cunningham, U.S. Bureau of Mines Bulletin 1985, 675, 185.  5) F.W. Miller, R.J. Fantel, D.A. Buckingham, U.S. Bureau of Mines Information 1986, Circular 9085, 20. 6) G. Amil, M. Ramanaji, M.R.P. Reddy, Arbind Kumar, T.L. Prakash, V.C. Sethi, Atomic Spectroscopy 2002, 23, 32. 7) S.M. Pyle, J.M. Nocerino, S.N. Deming, J.A. Palasota, Environ. Sci. Technol. 1996, 30, 204. 8) A. Johnson, G.C. Lalor, H. Robotham, M.K. Vutchkor, J. Radioanal. Nucl. Chem. 1996, 209, 101.  9) E.I. Obiajunwa, Nuclear Instrum. Methods in Physics Research B 2001, 184, 437. 10) T.T. Chao, R.F. Scanzolono, J. Geochemical Exploration 1992, 44, 65. 11) Z.Sulcek, P. Povondra, C.R.C., Inc. 1989.  12) R. Klockenkamper, Total reflection X-Ray Fluorescence Analysis, Wiley Inc. 1997. atti di euroconference on university and enterprise

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Characterisation of Columbite-Tantalite (Coltan) ore from Congo. Elemental composition by total reflection X-ray fluorescence analysis

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