Optical Stimulated Luminescence

In summary, when measuring an OSL spectrum, the stimulation source always has a higher wavelength than the emission of the material. This is because at lower wavelengths, the distinction between stimulation and emission light becomes difficult. Electron traps in thermo-luminescent materials can be released by its own luminescence, where luminescent centers in the crystal are ionized and the released electrons can be trapped again by infrared light in an OSL experiment. If a released electron from a trap is absorbed by a luminescent center, it can generate a photon with enough energy to release another trapped electron. However, this can only happen if there are available levels and the transition is allowed.
  • #1
ctydtgat
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In a measurement of an OSL spectrum the wavelength of the stimulation source is always higher than the wavelength of the emission of the material.
Is this due to the fact that at lower wavelengths one can no longer distinguish between stimulation and emission light?
Can electron traps be released by its own luminescence?

Thanks!
 
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  • #3
In a thermo-luminescent material there are electron traps just below the conduction band and there are impurity luminescent centers in the crystal, e.g. Eu, Ce, ...
After UV illumination of the material, luminescent centers (Eu, ..) can be ionized (Eu2+ -> Eu3+) and the released electron will be delocalized through the conduction band where it can be trapped into a trap just below the conduction band. In an OSL experiment these electrons can be released by illuminating the material using infrared, just enough energy to release it from the trap back to the conduction band.
Assume now that at a certain position an electron is indeed released from its trap. Then the electron can go to a luminescent center (Eu3+ + e -> Eu2+,*) which we assume for now to decay radiatively (there is also the possibility to decay non-radiatively). Then this particular center will generate a photon. This photon travels through the material where it could be absorbed by another trapped electron which will thus escape from its trap. However, the energy from the released photon due to Eu2+,* -> Eu2+ + photon is higher. So if the photon would be absorbed by another trapped electron this means that it would get energy rather high into the conduction band. If there are levels available and the transition is allowed, this could in principle happen I guess.
Does this makes sense?
 

Related to Optical Stimulated Luminescence

1. What is Optical Stimulated Luminescence (OSL)?

Optical Stimulated Luminescence (OSL) is a dating technique used in geology and archaeology to determine the age of sediments and materials. It measures the amount of light emitted from minerals in response to exposure to natural radiation, such as sunlight, and can provide dates for materials up to 100,000 years old.

2. How does OSL dating work?

OSL dating measures the amount of trapped electrons in minerals, such as quartz and feldspar, that have been exposed to natural radiation. These trapped electrons accumulate over time and are released when the minerals are exposed to light, producing a measurable light signal. The amount of light emitted is proportional to the length of time the minerals have been buried, allowing scientists to determine the age of the sample.

3. What are the advantages of using OSL dating?

OSL dating has several advantages over other dating techniques. It can be used to date a wide range of materials, including sediments, pottery, and burnt stones, and can provide accurate dates for materials up to 100,000 years old. It is also non-destructive, meaning that the sample does not need to be destroyed in order to obtain a date.

4. What are the limitations of OSL dating?

One limitation of OSL dating is that it can only be used to date materials that have been exposed to natural radiation, such as sunlight. This means it cannot be used to date materials that have been stored in the dark, such as deep cave sediments. Additionally, OSL dating is not suitable for materials younger than 100 years old, as the amount of trapped electrons may not be significant enough to produce a measurable light signal.

5. How is OSL dating used in scientific research?

OSL dating is a valuable tool in scientific research, particularly in geology and archaeology. It can provide accurate dates for sediments and materials, allowing scientists to better understand past environmental and geological processes. In archaeology, OSL dating can help determine the age of artifacts and provide a timeline for human occupation of a site. It is also used in geological studies to reconstruct past climate and landscape changes.

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