That is a phenomenal article. Gentry was actually doing experiments. Give him serious credit for this!
Gentry’s own attempts to duplicate alpha particle damage in minerals using a helium ion beam illustrates this problem. An ion beam irradiates an “area” and has luminosities (particles per beam cross section per unit time) many orders of magnitude higher than the “spherical” volumetric emission of alpha particles from radioactive centers in mineral grains. Short exposure to an ion beam can create damage patterns equivalent to millions of years of low-level natural alpha exposure. Gentry (1974) notes the problem of beam intensity required to achieve a specific level of discoloration. In these experiments, the ion beam intensity was adjusted to produce a discoloration pattern in the irradiated mineral, with the extent (or depth) of the discoloration then being compared to the measured halo diameters in his thin section specimens. The pattern produced by Gentry through ion beam bombardment was a zone of discoloration, faintest near the source, and increasing in intensity up to a relatively sharp termination. Gentry’s ion-beam work, however, was not able to produce multiple bands or the sharply defined concentric ring structure of certain haloes. It is likely that intense alpha particle bombardment disrupts the crystallinity of the target mineral (a well known natural radiation effect), changing its physical properties along the particle path. This would tend to broaden the Bragg Effect rather than creating a narrow zone of disruption (that is, a “ring”).
And points to some really interesting open questions:
Odom and Rink (1989) examined giant radiohaloes in mica and proposed an alternative hypothesis for their formation. They compare the circular halo structures in mica with radiation-induced color halos (RICHs) in quartz. In the quartz crystalline structure, aluminum can occasionally substitute for a silicon atom, creating a slight charge imbalance. Alpha particles from uranium decay create hole-trapping centers around the aluminum atoms. This in turn creates a semi-conductive area where beta particles (also resulting from uranium decay) can cause diffusion and discoloration over a fairly large area. The width of the resulting halo can be correlated with migration of valence-band holes along a radiation-induced charge potential in the host crystal. While this is an attractive hypothesis, Odom and Rink cautiously note that the crystal structures and chemical composition of quartz and mica are significantly different. Quartz is known to have natural piezoelectric properties missing in the mica group minerals. Without further investigation, haloes caused by migrating hole trapping centers is speculative for minerals other than quartz.
Clearly, more work is required to resolve all of these questions. The association of ring-type haloes with any specific energy of alpha decay must be considered speculative.


