Developing a predictive
understanding of mineral-phase stability
in extreme chemical conditions such as those found in nuclear waste
is challenging given the unknown influence of ionizing radiation.
The long-term impacts of cumulative radiation damage in the solid
state and exposure to radiolysis products in solution can impact mineral
precipitation, dissolution, and aggregation behavior. Here, we sought
to disentangle some of these effects by examining the dissolution
of gibbsite platelets in NaOH solutions using atomic force microscopy
with an integrated X-ray source that was used to compare dissolution
rates when particles were initially irradiated in a dry state versus
irradiated in solution, both of which were compared to unirradiated
controls. By tracking particle morphology changes and quantifying
material lost over time, dissolution rates and particle roughness
were found to be enhanced most when irradiation was carried out during
dissolution in NaOH, and to a lesser but significant extent when irradiated
dry prior to dissolution. The maximum observed dissolution enhancement
in the former case suggests the importance of both a direct effect
of absorbed dose on gibbsite stability and an indirect effect arising
from surface interaction with solution radiolysis products.