TL/OSL

- Luminescence dating -

Determines the total accumulated dose of radiation absorbed by a ceramic, stone or a mortar since their heating or exposure to sunlight.

WHAT IS IT FOR

dating

morphology

technology

origin

composition

alteration

APPLICABLE MATERIALS

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).

BRIEF DESCRIPTION

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).

Metrics

  • accuracy

  • time

  • cost

Sampling

in situ

invasive

destructive

TIPS

Advantages

  • only few samples are needed for one structure

Limitations

  • long process measurements
  • medium accuracy  

HOW DOES IT WORK?

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).

References