What is luminescence?
Bombarbing some form of energy at the surface of materials may result in the emission of radiation, other than heat, in the visible (400-700 nm), UV (<400 nm) or IR (>700 nm) - this is luminescence
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Luminescence has 2 components:
Phosphorescence - radiation that continues to emit after the incident energy is turned off (>10-8 sec)
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Phosphorescence example: The hands of the clock are painted with a phosphorescent ink, which absorbs light when illuminated and then radiates that light back out Source: http://www.glassner.com/andrew/cg/research/fluphos/fluphos.htm |
Fluorescence - radiation that stops after the incident energy is turned off (there are many examples of fluorescence in minerals)
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On the left is a
room lit first by a normal indoor incandescent bulb; we can see things
pretty well. (Note that the display dithering is not part of the original
image). Then we turn off the bulb and turn on a "black light", which is
really just a bulb that illuminates mostly in the blue and ultraviolet.
Notice that almost everything goes blue (or black) except for the posters,
which are painted with fluorescent ink. Those inks absorb the
short-wavelength blue light, and re-radiate the energy at the longer green
and yellow wavelengths. Without fluorescence, the posters would appear as
blue as the rest of the room, rather than colored. Source: http://www.glassner.com/andrew/cg/research/fluphos/fluphos.htm |
The forms of incident energy:
Electrons (cathodoluminescence[CL])

UV photons — black light (photoluminescence) - e.g. fluorescence in minerals
Ions (ionoluminescence)
X-rays, (roentgenoluminescence)
Triboluminescence (mechanical crushing) — e.g. Wintergreen Lifesavers or scratching sphalerite)
Thermoluminescence (heat)
Chemiluminescence (chemical reactions)
Bioluminescence (reactions in organisms)
Cathodoluminescence (CL)
visible light (400-700 nm) that is produced with the bombarding of material with energetic electrons
typically produced by the electron beam produced by an electron microprobe or SEM, or by cathodoluminescence microscopy attachment (CMA)
the nature of CL in material is a complex function of composition, lattice structure and superimposed strain or damage on the structure of the material
semi-quantitative, at best, but lots of information of material development

Electron beam bombardment

Interactions of the electron beam and sample
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Qualitative image of the interaction of an electron beam with a flat solid. Beam diameter (d) is typically 1-2 mm. Due to interactions with the solid, only secondary electrons near the surface will be emitted - small volume observed by SEM detector i.e. good for surface features. Backscattered electrons are emitted over a large volume and are a function of the mean atomic weight of the materials. X-rays are produced over a larger volume, assuming the excitation potential is above the appropriate level. The enlarged volume is a quantitative analyses limit of resolution. CL is commonly excited at greater depths (L), commonly 2-8 mm. This further reduces the resolution. (modified after Marshall, 1988; Beaman and Isasi, 1972) |
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Luminescence involves excitation of an electron to a state of higher energy and then a return to the low energy state accompanied by the emission of a photon |
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Depends on the electron configuration and the lattice that holds the element or ion. |
Causes of cathodoluminescence
Two types of CL:
Intrinsic luminescence - characteristic
of the host lattice - due to non-stoichiometry (vacancies), structural
imperfections (poor ordering in the crystal,
radiation
damage, shock damage) and impurities (non-activators that distort the
lattice.
Extrinsic luminescence - results from impurities - the impurities generate luminescent centers - most commonly transition elements, REEs and actinides.
Impurities – most common source of CL in minerals
Activators - trace elements (substitutional) that promote CL function of concentration such that CL increases to a point and then decreases (self-quenches) dependent on the lattice structure
Examples of activators: Mn2+, Fe3+, Ti4+, REE and others
Sensitizers (co-activators) – ions that must coexist with another impurity to luminescence. E.g. Pb2+ and Mn2+ produce in calcite to produce UV luminescence
Quenchers – ions that inhibit or eliminate CL in a mineral e. g. especially Fe2+
Instruments used for observation of CL
CL microscope attachment (CMA)
cold cathode — discharge takes place between the cathode and anode in an ionized gas (most common)
electron beam generated during discharge between cathode and anode in ionized gas (lower vacuum)
low intensity of silicate CL
film recording

hot cathode – electrons emitted by a heated filament
higher vacuum (<10-5 mbar)
14 keV accerating potential
electrons from heated filament
stable beam and greater CL intensity

2. SEM-CL
attachment to SEM
sequential RGB images
post-acquisition processing
stable beam and greater CL intensity
