Presentation on theme: "Cathodoluminescence Electron probe microanalysis EPMA Modified 11/10/08."— Presentation transcript:
Cathodoluminescence Electron probe microanalysis EPMA Modified 11/10/08
What’s the point? Some materials, when excited by electrons, produce certain ‘secondary’ electron excitation which then releases small quanta of energy in the range of a few eV…which translated into wavelengths, is the visual light spectrum. CL images can yield valuable information not easily seen by other means.
What it’s not Photoluminescence: radiation caused by excitation by UV or visible light (1.8 to 4.9 eV) Nor Phosphorescence: radiation that persists after the incident energy source is turned off But it is under the general category of Fluorescence, which is where the radiation ceases immediately (within sec) following cessation of the source.
Cathodoluminescence This is an optical (visible/nearly visible light) phenomenon. CL occurs in semiconductors/insulators, be they man- made or natural. Electrons in the valence band of these materials are excited into the conduction band for a brief time; subsequently these electrons recombine with the holes left in the valence band. The energy difference is released as a photon of wavelength of light. Two commonly used applications are (1)Locating strain (lattice mismatch) in semiconductors, and (2)Evaluating minerals for heterogeneous growth (complex history, overgrowths, dissolution, crack infilling).
Seeing The Light There are two distinct methods to image this effect: by SEM or microprobe, or by a small attachment to an optical microscope (static cold cathode electron source). Additionally, the light spectra can be quantified by a scanning monochronometer.
CL: in living color CL captured on color film: A: Casserite, SnO 2 B: Crinoidal limestone C: Red = dolomite, orange = calcite; dark grey = baddeleyite (ZrO 2 ) D: St Peter Sandstone; mature quartz with zoned authigenic quartz overgrowths (from Marshall,1988, CL of Geological Materials) D C B A The CL emitted is of varying wavelengths (=colors), and can be captured with the right equipment. Various “CL microscope attachments” have been built that fit on the stage of a regular microscope; one model is the (cold cathode) Luminoscope. EXAMPLES
(Cold) CL Microscope Attachments CMAs are relatively inexpensive attachments to microscopes. A high voltage (10-30 keV) cold cathode gun discharges electrons in a low vacuum chamber (rough pump only). A plasma results that provides charge neutralization (no carbon coating necessary). A camera (film or digital) and/or monochrometer are attached to acquire images and/or wavelength scans of the light. (From Marshall, 1993,The present state of CL attachments for optical microscopes, Scanning Microscopy, Vol 7, p. 861) Cold cathode gun
SEM/EP CL detectors Above: PM on SX51 Top Right: Gatan PanaCL on Hitachi: mirror inside chamber, inserted to operating position directly below pole piece; Below Right: PM with filters outside chamber
This figure demonstrates several different mechanisms whereby photons are emitted in the process of high voltage electrons promoting valence electrons to conduction band. CL: ‘jumping the band gap’
The various band gap energies with their respective wavelengths and colors is shown here. (image from Marshall, 1988, Fig 1.4, p. 4) CL: colors and eV
One term in common usage is “intrinsic CL”, which is meant to mean that some minerals inherently emit CL, e.g. that nearly all silicates have CL in the blue region. However, this is not a totally satisfactory statement. Intrinsic CL can be enhanced by non-stoichiometry structural imperfections – poorly ordered – radiation damage – shock damage impurities, substitutional or interstitial, which distort the lattice Theories about CL Note: these modify the bonds and electronic structure.
Substitution of an element for the ‘usual’ one (e.g. Ti 4+ for Si 4+ in quartz, Mn 2+ for Ca 2+ in calcite) is believed to be a key cause of distortion of the lattice (=a defect) in the mineral. Impurities which function thusly are called “activators”. A few elements can perform the opposite role: modify the energy level arrangement so that the CL process does not operate or is diminished. These are “quenchers”, with Fe 2+ being the most common. If the quencher level is low, it is possible that only a few ppm (or 50 ppb) of an activator is enough for CL emission. Impurities: activators/quenchers
It has been observed that CL intensity generally increases with increasing abundance of the activator ion, reaches a maximum and then “there is too much of a good thing” and the CL decreases as the activator level increases. The maximum CL intensity seems to occur when the activator level is in the wt level; e.g. CL intensity in doped feldspars is maximum at ~1.5 wt% Fe 3+ or Mn 2+. Too much activator?
A given mineral can accept different activators, and a give out a different CL color for each: feldspars can accept Eu 3+ - blue, Mn 2+ - greenish yellow, and Fe 3+ - red. A given activator may be incorporated by different minerals, and produce different colored CL in them: e.g. Mn 2+ can be accepted by feldspars - greenish yellow, apatite - yellow, and carbonates - reddish-orange. Several of the REE activators (e.g., Dy 3+, Sm 3+, Eu 3+ ) produce very sharp ‘line’ spectra whose wavelength is almost independent of the host mineral, and can be used to qualitatively analyze the element content. Pretty Colors
CL spectra Goetze, 2002
The intensity of CL can be altered by changing the sample temperature; there apparently are examples for increased intensity (in different materials) with both higher and lower temperatures. It has been shown that quartz CL can be enhanced by cooling the sample. Temperature effects
The intensity of CL can deteriorate with time under electron beam bombardment, and is called ‘electron beam aging’ in the phosphor industry. However, this is not believed to be a serious issue “under normal beam conditions and viewing times”. It has been reported to occur in quartz, over tens of seconds, and Time dependent effects that there is a color change from blue to red. Goetze, 2002
It is also obvious that SEMs with ‘normal vacuums’ with oil backstreaming easily cover the sample with a very thin coat of carbon which reduces the intensity of the detected CL. Thus one takes a low mag image first, and high mag last, else the small ‘carbon contamination’ rectangle will sit in the middle of the low mag image, not desirable. Time dependent effects
Visualize the distribution of different phases that are otherwise similar, e.g. calcite and dolomite; 2 feldspars in granite Pinpoint the presence and location of small or rare minerals in a rock e.g. apatite in granite Applications-for optical microscopy where no SEM-BSE available Applications where SEM-BSE available Determine that different regions of the same mineral have a complicated history -- growth zonation; dissolution surfaces; healed cracks, e.g. carbonates, quartz, zircon, feldspar
CL: defects in GaAs GaAs on Si for optoelectronic devices can have defects due to lattice mismatch between the film and Si substrate. The defects are not seen in SE image (top left). However, a CL image (bottom left) shows the areas of reduced strain, where a monochronometer collected 800 nm light. The right figure shows the CL spectra of strained (top) vs unstrained (bottom) material. Peter Heard, 1996, Cathodoluminescence--Interesting phenomenon or useful technique? Microscopy and Analysis, January, p These and the following CL images are mono- chromatic: only the total light intensity at each pixel is recorded by a photomultiplier. This is a common (simple/cheap) attachment for an SEM or microprobe.
CL: quartz, zircon Images acquired with the Cameca CL (PM) detector. Left: quartz from Skye with complex history of growth or re-equilibration with hydrothermal system. Trace amounts of Al, Ti or Mn may be involved. Right: CL image of zircon from Yellowstone tuff (false color); adjacent BSE image (no zonation obvious). BSE CL (from research of Valley, and Bindeman and Valley)
Here is a sample of an olivine rich chondrule from the Semarkona meteorite which contains unusual forsterite grains (dark grey BSE) that show both blue and red CL, enclosed in Al, Ca-rich glass (light grey BSE). Blue CL olivine at the rim is depleted in FeO (Fo>99.5) and enriched and enriched in refractory elements such as Al and Ca, while red CL olivine at core is slightly FeO-richer (Fo<99.5). Oxygen three isotope compositions of blue forsterite and glass are enriched in 16 O relative to red forsterite. Note the glass emits green CL. CL CL image Using CL to Provide Necessary Details to Explain SIMS Isotope Data Kita et al. (2007b) LPSC Abstract #1791
One problem with some materials is that the luminescence has a finite persistence, so that a typical SEM scan causing streaking, as shown above left when dolomite (CaMg- carbonate) is imaged by SEM-CL (using no filter). Reed and Milliken showed that dolomite emits CL in 2 broad bands, one red and the other UV-violet, and that using a blue (transmission) filter elimated the red light which was causing the streaking. The above right image was acquired with a UV-blue filter. (20 kV) CL Carbonate CL with SEM…using filters Reed and Milliken, 2003
CL Fournelle et al AGU 2000 CL Sector zoning in Yellowstone Pre-LCT zircon Bright CL: high P (and lower Y, U and Th) Dark CL: high Y, U, and Th (compared to Bright CL area) Y P Th U Trace elements quenching CL
Many (all?) epoxies produce CL: in color, dull green or blue. There are some minerals where any CL is totally quenched, and in grain mounts, the crystal is black CL surrounded by brighter epoxy! Common lapping and polishing abrasives (diamond, alumina, silicon carbide) emit CL! The sample must be well cleaned by ultrasonic treatment prior to examination Uncovered common glass microscope slides emit a dull blue CL CL Sample Prep: Epoxy and Abrasive In this false-colored monochrome image, the epoxy is emitting significant CL, intermediate in intensity to the zones in the zircon!
CL Cathodoluminescence image of zircon from Yakutian kimberlite (Russia) shows inherited core with thin oscillatory zoning overgrown by a homogeneous rim. Found on Web: Source, Bill Griffin, Elena Belousova; funded by Rio Tinto, BHP, Macquarie University
CL Class I: Native elements Diamond Class II: Sulfides Sphalerite ZnS (important in phosphor industry) Cinnabar HgS Realgar AsS Class III: Oxides Periclase MgO Spinel MgAl2O4 (synthetic only) Corundum, Ruby, Sapphire Al2O3 Cassiterite SnO2 CL in common minerals* -1 * Short list. Complete list in Marshall 1988
CL Class IV: Halides Halite NaCl Fluorite CaF2 Class V: Carbonates Calcite and Aragonite CaCO3 Rhodochrosite MnCO3 Witherite BaCO3 Strontianite SrCO3 Cerussite PbCO3 CL in common minerals* -2 * Short list. Complete list in Marshall 1988
CL Class VI: Sulfates, Tungstates Barites BaSO4 Anhydrite CaSO4 Gypsum CaSO4-2H2O Scheelite CaWO4 (a common EPMA focus mineral) Class VII: Phosphates Apatite (Ca5(P)4)3(F,Cl,OH) Class VIII: Silicates Quartz, Chalcedony, Tridymite, Cristobalite SiO2 Feldspars CL in common minerals* -3 * Short list. Complete list in Marshall 1988
CL Class VIII: Silicates-continued Scapolite Kaolinite Serpentine Muscovite Tremolite Spodumene Wollastonite Benitoite BaTiSi3O9 - another EPMA bright light Beryl CL in common minerals* - 4 * Short list. Complete list in Marshall 1988
CL Class VIII: Silicates-continued Cordierite Epidote Olivine (Fe-free) Andalusite, Sillimanite, Kyanite Al2SiO5 Garnets - limited sightings Zircon CL in common minerals* - 5 * Short list. Complete list in Marshall 1988