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    Osl dating sediments

    Two approaches result in OSL ages that are internally consistent and in excellent agreement with radiocarbon dating, indicating that all investigated sediments are younger than AD 1500.From this data a complex deposition and incision history is constructed for the last 500 years.Des datations par OSL (Optically Stimulated Luminescence) sont utilisées pour reconstituer la chronologie de phases d’aggradation et d’incision dans un sous-bassin élémentaire du bassin de l’Yzeron (France).Différents traitements statistiques visant à extraire les doses équivalentes moyennes des distributions des doses sont comparés pour estimer l’effet de la variété du blanchiment du signal OSL antérieur au dépôt.

    Two short-lived phases of incision during the first half of the XIX century were probably caused by a decrease of sediment supply due to a decline in the frequency of heavy precipitation events.

    The radiation causes charge to remain within the grains in structurally unstable "electron traps".

    The trapped charge accumulates over time at a rate determined by the amount of background radiation at the location where the sample was buried.

    The ionizing radiation produces electron-hole pairs: Electrons are in the conduction band and holes in the valence band.

    The electrons that have been excited to the conduction band may become entrapped in the electron or hole traps.

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