- Luminescence dating -
Determines the total accumulated dose of radiation absorbed by a ceramic, stone or a mortar since their heating or exposure to sunlight.
dating
morphology
technology
origin
composition
alteration
Ceramic
Mortar
Stone
Ceramic Building Materials (CBM), Mortar & Plaster, Stone
The technique may be applied to Ceramic building materials (CBM), i.e. bricks, tiles, to mortars and, in some cases, to stones (few examples for this application, which is very difficult to set up notably to retrieve the minerals).
TL signals (intensity vs stimulation temperature)
Some minerals such as quartz or feldspars, typically found in ceramic materials, stone or mortars absorb and store a radiation dose* originating from the effects of the surrounding radioactivity. When bricks or tiles are fired during their manufacturing or when sand is exposed to the sun before its addition to lime, the radiation dose of geological origin is removed. From this moment, considered as the resetting of the brick or mortar, the chronometer mechanism starts: the grains
increasingly accumulate a new radiation dose again, known as ‘paleodose’.
The dating method consists in measuring the archaeological dose in the lab by heating (“thermo-“, TL) or lighting (“optically stimulated”, OSL) the crystals*. This leads to the emission of photons (“luminescence”), the intensity of which is proportional to the Paleodose. The environmental contribution to the annual dose is measured on site and the contribution from the sample itself in the lab (Bailiff , 2007).
accuracy
time
cost
in situ
invasive
destructive
Some minerals such as quartz or feldspars, typically found in ceramic materials, stone or mortars absorb and store a radiation dose* originating from the effects of the surrounding radioactivity. When bricks or tiles are fired during their manufacturing or when sand is exposed to the sun before its addition to lime, the radiation dose of geological origin is removed. From this moment, considered as the resetting of the brick or mortar, the chronometer mechanism starts: the grains increasingly accumulate a new radiation dose again, known as ‘paleodose’.
The dating method consists in measuring the archaeological dose in the lab by heating (“thermo-“, TL) or lighting (“optically stimulated”, OSL) the crystals*. This leads to the emission of photons (“luminescence”), the intensity of which is proportional to the Paleodose. The environmental contribution to the annual dose is measured on site and the contribution from the sample itself in the lab (Bailiff , 2007).