Thermoluminescence dating TL is the determination, by means of measuring the accumulated radiation dose, of the time elapsed since material containing crystalline minerals was either heated lava , ceramics or exposed to sunlight sediments. As a crystalline material is heated during measurements, the process of thermoluminescence starts. Thermoluminescence emits a weak light signal that is proportional to the radiation dose absorbed by the material. It is a type of luminescence dating. Sediments are more expensive to date. It will often work well with stones that have been heated by fire.
In thermoluminescence dating, these long-term traps are used to determine the age of materials: When irradiated crystalline material is again heated or exposed to strong light, the trapped electrons are given sufficient energy to escape.
1: phosphorescence developed in a previously excited substance upon gentle heating. 2: the determination of the age of old material (such as pottery) by the amount of thermoluminescence it . Figure 4: Illustrated method of passively monitoring sand input (Keizars, ). Thermoluminescence (TL) dating is the determination, by means of measuring the accumulated radiation dose, of the time elapsed since material containing crystalline minerals was either heated (lava, ceramics. Thermoluminescence dating definition, a method of dating archaeological specimens, chiefly pottery, by measuring the radiation given off by ceramic materials as they are heated. See more.
In the process of recombining with a lattice ion, they lose energy and emit photons light quantadetectable in the laboratory. The amount of light produced is proportional to the number of trapped electrons that have been freed which is in turn proportional to the radiation dose accumulated.
Thermoluminescence dating is the determination, by means of measuring the accumulated radiation dose, of the time elapsed since material containing crystalline .
In order to relate the signal the thermoluminescence-light produced when the material is heated to the radiation dose that caused it, it is necessary to calibrate the material with known doses of radiation since the density of traps is highly variable. Thermoluminescence dating presupposes a "zeroing" event in the history of the material, either heating in the case of pottery or lava or exposure to sunlight in the case of sedimentsthat removes the pre-existing trapped electrons.
Therefore, at that point the thermoluminescence signal is zero.
As time goes on, the ionizing radiation field around the material causes the trapped electrons to accumulate Figure 2. In the laboratory, the accumulated radiation dose can be measured, but this by itself is insufficient to determine the time since the zeroing event.
The Radiation Dose Rate - the dose accumulated per year-must be determined first. This is commonly done by measurement of the alpha radioactivity the uranium and thorium content and the potassium content K is a beta and gamma emitter of the sample material.
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Often the gamma radiation field at the position of the sample material is measured, or it may be calculated from the alpha radioactivity and potassium content of the sample environment, and the cosmic ray dose is added in.
Once all components of the radiation field are determined, the accumulated dose from the thermoluminescence measurements is divided by the dose accumulating each year, to obtain the years since the zeroing event. Thermoluminescence dating is used for material where radiocarbon dating is not available, like sediments.
Its use is now common in the authentication of old ceramic wares, for which it gives the approximate date of the last firing. An example of this can be seen in Rink and Bartoll, Thermoluminescence dating was modified for use as a passive sand migration analysis tool by Keizars, et al. Optically stimulated luminescence dating is a related measurement method which replaces heating with exposure to intense light.
The sample material is illuminated with a very bright source of green or blue light for quartz or infrared light for potassium feldspars. Ultraviolet light emitted by the sample is detected for measurement.
TL testing is a dating method for archaeological items which can distinguish between genuine and fake antiquities. All translations of Thermoluminescence dating.
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