ALL SEX DATING
clear and disable history
Strengths and limitations of radiocarbon dating
-counting method) or by directly counting the radiocarbon atoms using a method called Accelerator Mass Spectrometry (AMS).Measurement of the radioactivity of the sample works very well if the sample is large, but in 9 months less than 0.01% of the radiocarbon ions will decay, so in a reasonable measurement time (typically a few weeks) only a very small proportion of the radiocarbon atoms are detected by this method.AMS, on the other hand, can in principle detect a much higher proportion (typically about 1% of the total) allowing sample sizes to be smaller by a factor of about a thousand.
It is ionised by bombarding it with caesium ions and then focused into fast-moving beam (energy typically 25ke V).The ions produced are negative which prevents the confusion of ions). As they travel to the terminal (which is at about 2MV), they are accelerated so much that when they collide with the gas molecules in the central `stripper canal'.All of the molecular ions (such as Careful sampling and pre-treatment are very important stages in the dating process, particularly for archaeological samples where there is frequently contamination from the soil.Before sampling, the surface layers are usually removed because these are most susceptible to contamination.Only very small quantities are required for the AMS measurement (30ug-3mg of carbon) and so the damage to objects can be minimised.The chemical pre-treatment depends on the type of sample.As an example bones are treated as follows: Several of these procedures are done in an automated continuous flow system.After chemical pre-treatment, the samples are burnt to produce carbon dioxide and nitrogen.A small amount of this gas is bled into a mass spectrometer where the stable isotope ratios of carbon and nitrogen are measured.These ratios provide useful information on the purity of the sample and clues about the diet and climatic conditions of the living organism.The carbon isotope ratio can also be used to correct for isotopic fractionation in the radiocarbon measurement.