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Thanks to nuclear physics, mass spectrometers have been fine-tuned to separate a rare isotope from an abundant neighboring mass, and accelerator mass spectrometry was born.

A method has finally been developed to detect carbon 14 in a given sample and ignore the more abundant isotopes that swamp the carbon 14 signal.

At this stage, molecules that may be present are eliminated because they cannot exist in this triple charged state.

The carbon atoms with triple positive charge further accelerate away from the positive terminal and pass through another set of focusing devices where mass analysis occurs.

There are essentially two parts in the process of radiocarbon dating through accelerator mass spectrometry.

The first part involves accelerating the ions to extraordinarily high kinetic energies, and the subsequent step involves mass analysis.

These two radiocarbon dating methods use modern standards such as oxalic acid and other reference materials.

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Accelerator mass spectrometry also takes less time to analyze samples for carbon 14 content compared to radiometric dating methods that can take one or two days.

From these data, concentration ratio of the isotopes can be known to allow evaluation of the level of fractionation.

The greatest advantage that AMS radiocarbon dating has over radiometric methods is small sample size.

There are two accelerator systems commonly used for radiocarbon dating through accelerator mass spectrometry.

One is the cyclotron, and the other is a tandem electrostatic accelerator.

After pretreatment, samples for radiocarbon dating are prepared for use in an accelerator mass spectrometer by converting them into a solid graphite form.

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