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Hyperspectral Cathodoluminescence Imaging and Analysis Extending from Ultraviolet to Near Infrared

Published online by Cambridge University Press:  20 November 2012

C.M. MacRae*
Affiliation:
Microbeam Laboratory, CSIRO Process Science and Engineering, Clayton, 3168, Victoria, Australia
N.C. Wilson
Affiliation:
Microbeam Laboratory, CSIRO Process Science and Engineering, Clayton, 3168, Victoria, Australia
A. Torpy
Affiliation:
Microbeam Laboratory, CSIRO Process Science and Engineering, Clayton, 3168, Victoria, Australia
C.J. Davidson
Affiliation:
Microbeam Laboratory, CSIRO Process Science and Engineering, Clayton, 3168, Victoria, Australia
*
*Corresponding author. E-mail: colin.macrae@csiro.au
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Abstract

The measurement of near-infrared (NIR) cathodoluminescence (CL) with sufficient sensitivity to allow full spectral mapping has been investigated through the application of optimized grating spectrometers that allow the ultraviolet (UV), visible, and NIR CL spectra to be measured simultaneously. Two optical spectrometers have been integrated into an electron microprobe, allowing simultaneous collection of hyperspectral CL (UV-NIR), characteristic X-rays, and electron signals. Combined hyperspectral CL spectra collected from two natural apatite (Ca5[PO4]3[OH,F]) samples from Wilberforce (Ontario, Canada) and Durango (Mexico) were qualitatively analyzed to identify the emission centers and then deconvoluted pixel-by-pixel using least-squares fitting to produce a series of ion-resolved CL intensity maps. Preliminary investigation of apatite has shown strong NIR emissions associated primarily with the rare-earth element Nd. Details of growth and alteration were revealed in the NIR that were not discernable with electron-induced X-ray mapping. Intense emission centers from Nd3+ and Sm3+ were observed in the spectra from both apatites, along with minor emissions from other 3+ rare-earth elements. Quantitative electron probe microanalysis was performed on points within the mapped area of the Durango apatite to produce a calibration line relating cathodoluminescent intensity of the fitted peak centered at 1,073 nm (1.156 eV) to the Nd concentration.

Type
Special Section: Cathodoluminescence
Copyright
Copyright © Microscopy Society of America 2012

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References

Barbarand, J. & Pagel, M. (2001). Cathodoluminescence study of apatite crystals. Am Mineral 86(4), 473484.CrossRefGoogle Scholar
Barwood, H. (2007). Digital near-infrared (NIR) cathodoluminescence (CL) imaging and image processing. Am Mineral 92(2-3), 261266.CrossRefGoogle Scholar
Blanc, P., Baumer, A., Cesborn, F., Ohnenstetter, D., Panczer, G. & Remond, G. (2000). Systematic cathodoluminescence spectral analysis of synthetic doped minerals. In Cathodoluminescence in Geosciences, Pagel, M., Barbin, V., Blanc, P. & Ohnestetter, D. (Eds.), pp. 127160. Berlin, New York: Springer.CrossRefGoogle Scholar
Edwards, P.R., Martin, R.W., O'Donnell, K.P. & Watson, I.M. (2003). Simultaneous composition mapping and hyperspectral cathodoluminescence imaging of InGaN epilayers. Phys Stat Sol 7, 24742477.Google Scholar
Gaft, M., Reisfeld, R. & Panczer, G. (2005). Luminescence Spectroscopy of Minerals and Materials. Berlin, Heidelberg: Springer.Google Scholar
Gaft, M., Reisfeld, R., Panczer, G., Boulon, G., Shoval, S. & Champagnon, B. (1997). Accommodation of rare-earth and manganese by apatite. Opt Mater 8, 149156.CrossRefGoogle Scholar
Geake, J.E., Walker, G., Telfer, D.J. & Mills, A.A. (1977). Cause and significance of luminescence in lunar plagioclase. Phil T R Soc A 285(1327), 403408.Google Scholar
Gorobets, B.S. & Rogojin, A.A. (2002). Luminescent Spectra of Minerals. Moscow: All-Russia Institute of Mineral Resources.Google Scholar
Götze, J. (2000). Materials characterisation by cathodoluminescence microscopy and spectroscopy. In Proceedings of the Sixth International Congress on Applied Mineralogy in Research, Economy, Technology, Ecology and Culture, Göttingen, July 2000, pp. 783786.Google Scholar
Götze, J., Habermann, D., Neuser, R.D. & Richter, D.K. (1999). High-resolution spectrometric analysis of rare earth elements-activated cathodoluminescence in feldspar minerals. Chem Geol 153(1-4), 8191.CrossRefGoogle Scholar
Habermann, D., Gotte, T., Meijer, J., Stephan, A., Richter, D.K. & Niklas, J.R. (2000). High resolution rare-earth elements analyses of natural apatite and its application in geo-sciences: Combined micro-PIXE, quantitative CL spectroscopy and electron spin resonance analyses. Nucl Instrum Meth B 161, 846851.CrossRefGoogle Scholar
Harrowfield, I.R., MacRae, C. & Wilson, N.C. (1993). Chemical imaging in electron microprobes. In Proceedings of the 27th Annual MAS Meeting 1993, pp. 547548. Microbeam Analysis Society.Google Scholar
Kayama, M., Nakano, S. & Nishido, H. (2010). Characteristics of emission centers in alkali feldspar: A new approach by using cathodoluminescence spectral deconvolution. Am Mineral 95(11-12), 17831795.CrossRefGoogle Scholar
Kempe, U. & Götze, J. (2002). Cathodoluminescence (CL) behaviour and crystal chemistry of apatite from rare-metal deposits. Mineral Mag 66(1), 151172.CrossRefGoogle Scholar
MacRae, C.M. & Wilson, N.C. (2008). Luminescence database I—Minerals and materials. Microsc Microanal 14(2), 184204.CrossRefGoogle ScholarPubMed
MacRae, C.M., Wilson, N.C. & Brugger, J. (2009). Quantitative cathodoluminescence mapping with application to a Kalgoorlie scheelite. Microsc Microanal 15(3), 222230.CrossRefGoogle ScholarPubMed
MacRae, C.M., Wilson, N.C., Johnson, S.A., Phillips, P.L. & Otsuki, M. (2005). Hyperspectral mapping—Combining cathodoluminescence and X-ray collection in an electron microprobe. Microsc Res Techniq 67(5), 271277.CrossRefGoogle Scholar
Marfunin, A.S. (1979). Spectroscopy, Luminescence and Radiation Centers in Minerals. Berlin, Heidelberg, New York: Springer-Verlag.CrossRefGoogle Scholar
Marshall, D.J. (1988). Cathodoluminescence of Geological Materials. London: Unwin Hyman Ltd. Google Scholar
Murakami, S., Morita, M., Herren, M., Sakurai, T. & Rau, D. (2000). Near-infrared luminescence and spectral anomaly in PLZT ceramics doped with Nd3+, Er3+, Yb3+ and Cr5+ ions at low temperatures. J Luminesc 87–89, 694696.CrossRefGoogle Scholar
Pagel, M., Barbin, V., Blanc, P. & Ohnestetter, D. (2000). Cathodoluminescence in Geosciences. Berlin, New York: Springer.CrossRefGoogle Scholar
Remond, G., Phillips, M.R. & Roque-Carmes, C. (2000). Importance of instrumental and experimental factors on the interpretation of cathodoluminescence data from wide band gap materials. In Cathodoluminescence in Geosciences, Pagel, M., Barbin, V., Blanc, P. & Ohnenstetter, D. (Eds.), pp. 108113. Heidelberg: Springer Verlag.Google Scholar
Stevens-Kalceff, M.A. (2009). Cathodoluminescence microcharacterization of point defects in alpha-quartz. Mineral Mag 73(4), 585605.CrossRefGoogle Scholar
Stowe, D.J., Galloway, S.A., Senkader, S., Mallik, K., Falster, R.J. & Wilshaw, P.R. (2004). A room temperature cathodoluminescence study of dislocations in silicon. Elect Microsc Anal 2003(179), 6770.Google Scholar
Tarashchan, A.N. (1978). Luminescence of Minerals. Kiev, Ukraine: Naukova Dumka.Google Scholar
Waychunas, G.A. (2002). Apatite luminescence. In Reviews in Mineralogy and Geochemistry, vol. 48, Matthew, J.R., Kohn, L. & Hughes, J.M. (Ed.), pp. 701742. Mineralogical Society of America.Google Scholar