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That rate can be calibrated by experiment, thus removing one of the main assumptions inherent in most natural dating methods: the composition of the starting material.
Excavated materials prove difficult to date because of the different thermal environments of different loci.
Measuring temperatures of different depths in the field should be explored to counteract this limitation.
This technique is based upon dating the Stage II kinetics of the rehydroxylation process using a (time)1/4 power model.
The original rehydroxylation method utilised very expensive equipment so this experiment proposes a different measurement protocol that most university laboratories can implement easily.
Different levels of humidity have had a significant effect on mass gain, contrary to previous literature.