Arrhenius activation energy and transitivity in fission-track annealing equations
Matheus Rufino, Sandro Guedes

TL;DR
This paper develops a formalism to analyze fission-track annealing models, calculating rate constants and activation energies, and finds that fanning models best fit laboratory data and geological evidence, indicating complex recombination mechanisms.
Contribution
It introduces a formalism based on physicochemical quantities to interpret and compare different fission-track annealing models, highlighting the superiority of fanning models.
Findings
Fanning models fit laboratory data better and align with geological evidence.
Parallel models suggest a single activation energy mechanism.
Fanning models indicate complex, non-quantum energy barrier transitions.
Abstract
Fission-track annealing models aim to extrapolate laboratory annealing kinetics to the geological timescale for application to geological studies. Model trends empirically capture the mechanisms of track length reduction. To facilitate the interpretation of the fission-track annealing trends, a formalism, based on quantities already in use for the study of physicochemical processes, is developed and allows for the calculation of rate constants, Arrhenius activation energies, and transitivity functions for the fission-track annealing models. These quantities are then obtained for the parallel Arrhenius, parallel curvilinear, fanning Arrhenius, and fanning curvilinear models, fitted with Durango apatite data. Parallel models showed to be consistent with a single activation energy mechanism and a reaction order model of order ~ -4. However, the fanning curvilinear model is the one that…
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Taxonomy
TopicsGeological and Geochemical Analysis · Nuclear materials and radiation effects · Radioactive element chemistry and processing
