David L. Shuster

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        Research
4He/3He thermochronometry
proton-induced 3He

With Janet Sisterson (Northeast Proton Therapy Center, NPTC), and   Don Burnett (CIT), we demonstrated in our 2004 study that a spatially uniform distribution of 3He is produced within minerals when irradiated with an energetic (>100 MeV) proton beam produced by cyclotron acceleration.  Essentially all atoms present in a mineral can produce spallation 3He.

For our purpose, a uniform 3He distribution is useful primarily for two reasons:

(i) it enables a stepwise degassing experiment in which the natural
4He release fractions are normalized to the proton-induced 3He released in the same step:  the ratio evolution diagram constrains the natural 4He distribution within the sample, and

(ii) it satisfies the initial condition from which diffusion coefficients are easily calculated.

In our latest irradiation, we generated 109 atoms 3He/mg with a fluence of 1×1016 protons/cm2 at 220 MeV, accomplished with a beam current of ~280 nA over a single 8 hour period.  This is an enormous concentration of 3He which easily permits single grain analyses.