| INFRARED (IR) AND ULTRAVIOLET (UV) FLUORESCENCE The previous photos show various materials emitting visible light in response to excitation by LEDs (UV and visible). Many specimens do emit (fluoresce) invisible "light" in the IR as well. Chlorophyll, for example, emits strongly in the far red and near IR (685 nm and beyond) when excited in the near UV or blue. The dye Indocyanine Green has an absorption peak around 800 nm and an emission peak around 835 nm. That dye has been used for angiography employing video microscopy. CCD video cameras are very sensitive to IR out to approximately 1100 nm, if they do not have an IR blocking filter. This characteristic makes these relatively inexpensive cameras very useful for certain IR studies. Note should be taken that LEDs usually emit some radiation in the IR that needs to be blocked. This will prevent reflection of the radiation that could pass as IR fluorescence. Incidentally, some researchers have referred to infrared fluorescence as infrared luminescence. Unlike the terms x-ray fluorescence or UV fluorescence, infrared fluorescence usually denotes the emission, rather than the exciting, wavelengths. Below are several photographs of various minerals taken using visible light LEDs emitting in the blue-green to excite IR fluorescence, along with a video camera equipped with an IR-transmission filter to record the fluorescence. An IR-cutting filter (to filter out any extraneous infrared) was placed on the LED lamp. |
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A sample of greenockite, a rare mineral, from Llallagua, Potosi, Bolivia A cadmium sulfide encrustation on the rock matrix is visible. The blue-green LED infrared-fluorescence image was inserted into the red channel of a white-light photo of the specimen. |
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A fragment of synthetic ruby (Al2O3:Cr) producing very strong IR fluorescence Cruder but very effective specimens for fluorescence studies can be easily made by melting a mixture of aluminum oxide and chromium trioxide in a ceramic crucible in a laboratory carbon-arc setup. |
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Kyanite (Al2SiO5) exhibiting strong IR fluorescence Many specimens of kyanite from different locales exhibit IR fluorescence. This sample practically jumped out at me as I was screening specimens from my mineral collection. Unfortunately, the point of origin for this rock was not given. Very, very few minerals exhibit IR fluorescence well. One way of quickly screening specimens is to illuminate the rock with a green laser pointer (532 nm) and look for a bright spot on the monitor delineating good luminescent areas. If the rock doesn't pass this simple test, the chance for finding any fluorescence under ultrabright LEDs is practically nil. Another sample of kyanite from Imperial County, California, exhibited practically no emission in the infrared. |
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is a comparison between the use of LEDs in UV fluorescence versus a standard
mercury-lamp wand. In brief, LEDs do not currently emit light much below
~378 nm. As such, this prevents their use for examining minerals that
glow under short-wave only (e.g., scheelite). The next pair of photos
shows a sample of franklinite (so highly prized by collectors specializing
in fluorescent minerals) illuminated by a short-wave lamp (on the left)
and a UV LED (on the right). Clearly, LEDs have a secure place in the
lab, but they cannot completely replace mercury lamps. At least, not yet!
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| LEDs
are already quite suitable for special illumination applications in many
areas of science as a whole and microscopy in particular. On the next
few pages, some of the best and brightest LEDs currently available are
demonstrated being used on a new microscope I designed for the study of
microorganisms. |
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