Fractionalization dating how to

(DIC: measured, carb: carbonate dissolved (0‰), soil: soil air (-23‰) this simple model is also only strictly valid for closed conditions and does not take into account fractionation effects (low p H environments) more complex models taking into account the chemical and isotopic evolution have been developed (e.g.

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C at the Gif-sur-Yvette Tandetron AMS facility is described.

The geological significance of the element fractionation process depends on the understanding of that process.

A process that is fast relative to the time that has elapsed since then, can be ‘dated’.

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