RETROSPECTION OF U.S. NUCLEAR REGULATORY COMMISSION EFFORTS ON NATURAL ANALOGS AND THE PEÑA BLANCA URANIUM DISTRICT
NRC-funded work in the Peña Blanca district has focused on (1) characterization of processes important to oxidative alteration of uraninite, (2) characterization of processes important to subsequent migration of radioelements through silicic tuffs, and (3) modeling the processes which control uraninite alteration and radioelement migration. Field studies included geologic mapping, contact gamma surveys, collection of solid, vegetation, and water samples, and characterization of local hydrology. Laboratory investigations included analyses of mapping data, mineralogy, petrology, rock, plant and water chemistry, stable and radioisotope analyses, and hydraulic characterization of tuffs. These studies (http://www.swri.edu/4org/d20/ghs/PBlanca/index.html) have led to (1) a description of the alteration of uraninite that occurred over long time scales that is comparable to that observed in Yucca Mountain-approximate laboratory experiments of spent fuel degradation; (2) implementation of an alternate source term model for the NRC's performance assessment code; (3) a better understanding of radioelement mobility in fracture transport pathways; and (4) demonstration of episodes of elevated radionuclide mobility, likely related to increased water flow.
The NRC staff views expressed herein are preliminary and do not constitute a final judgment or determination of the matters addressed or of the acceptability of a license application for a geologic repository at Yucca Mountain.