At now fine grains method is applied in our laboratory, but in future also the quartz inclusion grains procedure will be implemented.
After an experimental comparison between chemical preparations of the samples reported in literature, the procedure described in  was adopted, being the one that gave the best results on objects of known age even if the material is of poor quality.
Otherwise, for greater accuracy and according to the availability of the material, a measurement by means of gamma spectroscopy (HPGe-ORTEC detector) can be performed.
Using gamma spectroscopy it is also possible an estimation of the radon loss.
The TL dating requires the measurement of two quantities: the total accumulated absorbed radiation dose in selected minerals (so-called palaeodose) and the annual dose due to the natural radioisotope content of the sample and its surrounding environment.
From these two measurements, the TL age can be subsequently calculated from the basic equation: age=(palaeodose)/(annual dose).
The facility, run by Dr Kira Westaway, contains a fully equip wet room preparation area with a core and tube opening station, HF fume hoods, wet and dry sieving and mineral separation stations, and a ball mill.
In this case 40-potassium amount is measured by means of ICP (Inductively Coupled Plasma).
Luminescence dating is a trapped charge technique whereby electrons are ‘trapped’ in defects in the minerals such as quartz and feldspar.
This trapped signal is light sensitive and builds up over time during a period of no light exposure (during deposition or burial) but when exposed to light (natural sunlight or artificial light in a laboratory) the signal is released from the traps in the form of light – called luminescence.
Luminescence dating is based on quantifying both the radiation dose received by a sample since its zeroing event, and the dose rate which it has experienced during the accumulation period.
The technique can be applied to a wide variety of heated materials, including archaeological ceramics, burnt stones, burnt flints, and contact-heated soils and sediments associated with archaeological or natural events.