Remote Raman and fluorescence studies of mineral samples.

In the present study, we investigated remote laser-induced fluorescence (LIF), at a distance of 4.8 m, of a variety of natural minerals and rocks, and Hawaiian Ti (Cordyline terminalis) plant leaves. These minerals included calcite cleavage, calcite onex and calcite travertine, gypsum, fluorapatite, Dover flint and chalk, chalcedony and nephelene syenite, and rubies containing rock. Pulsed laser excitation of the samples at 355 and 266 nm often resulted in strong fluorescence. The LIF bands in the violet-blue region at approximately 413 and approximately 437 nm were observed only in the spectrum of calcite cleavage. The green LIF bands with band maxima in the narrow range of approximately 501-504 nm were observed in the spectra of all the minerals with the exception of the nephelene syenite and ruby rocks. The LIF red bands were observed in the range approximately 685-711 nm in all samples. Excitation with 532 nm wavelength laser gave broad but relatively low fluorescence background in the low-frequency region of the Raman spectra of these minerals. One microsecond signal gating was effective in removing nearly all background fluorescence (with peak at approximately 610 nm) from calcite cleavage Raman spectra, indicating that the fluorescence was probably from long-lifetime inorganic phosphorescence.

[1]  Georges Boulon,et al.  Laser-induced time-resolved luminescence of minerals , 1998 .

[2]  Renata Reisfeld,et al.  Laser-induced time-resolved luminescence as a tool for rare-earth element identification in minerals , 2001 .

[3]  Georges Boulon,et al.  Laser-induced luminescence of rare-earth elements in natural fluor-apatites , 1996 .

[4]  M. Pagel,et al.  Cathodoluminescence in Geosciences , 2000 .

[5]  Shiv k. Sharma,et al.  Spectroscopy at very high pressures. X. Use of ruby R-lines in the estimation of pressure at ambient and at low temperatures , 1976 .

[6]  A. N. Mariano,et al.  Europium-activated cathodoluminescence in minerals , 1975 .

[7]  Paul G. Lucey,et al.  Remote Pulsed Laser Raman Spectroscopy System for Mineral Analysis on Planetary Surfaces to 66 Meters , 2002 .

[8]  D. F. Nelson,et al.  Coherence, Narrowing, Directionality, and Relaxation Oscillations in the Light Emission from Ruby , 1960 .

[9]  D. Peacor,et al.  Luminescence, color and fission track zoning in apatite crystals of the Panasqueira tin-tungsten deposit, Beira-Baixa, Portugal , 1985 .

[10]  D. J. Marshall,et al.  Cathodoluminescence of geological materials , 1988 .

[11]  E. Schlodder,et al.  Decay kinetics and quantum yields of fluorescence in photosystem I from Synechococcus elongatus with P700 in the reduced and oxidized state: are the kinetics of excited state decay trap-limited or transfer-limited? , 2000, Biophysical journal.

[12]  F. Mackenzie,et al.  Characterization of some biogenic carbonates with Raman spectroscopy , 1991 .

[13]  P. Lucey,et al.  Stand-off Raman spectroscopic detection of minerals on planetary surfaces. , 2003, Spectrochimica acta. Part A, Molecular and biomolecular spectroscopy.

[14]  Georges Boulon,et al.  Accommodation of rare-earths and manganese by apatite , 1997 .

[15]  L. Merkle,et al.  Spectra and energy levels of trivalent samarium in strontium fluorapatite , 1997 .