Ion exchange between aqueous fluid and spent nuclear fuel alteration products: Implications for the mobility of Cs in the probable repository at Yucca Mountain

摘要

Compreignacite, a naturally occurring potassium oxide hydrate, is an expected alteration product of spent nuclear fuel subjected to oxidative corrosion in the presence of water. Ion-exchange experiments were performed using natural crystals of compreignacite in a 2 M CsCl solution at 180 deg for 24 h, and in a 100 ppm CsCl solution at 90 deg for 14 days. Exchange of Cs into crystals of compreignacite was demonstrated by crystal-structure analysis for a crystal from 2 M solution and chemical analysis for crystals from both exchange experiments. The structure of Cs-exchanged compreignacite is hexagonal, space group P6-bar 2m, a = 14.1014 (18) A, c = 15.127(3)A, V = 2605.1(7) A~2. It was solved by direct methods and refined on the basis of F~2 for all unique reflections to a final R1=6.37 percent. The structure determination demonstrated almost complete exchange of Cs for K in the interlayer of the structure, as confirmed by confirmed by compositional of the crystals, and provided the formula Cs_6[(UO_2)_(12)(OH)_(10)O_(10)](H_2O)_3.5, Z = 2. The structure of Cs-exchanged compreignacite contains alpha-U_3O_8-type sheets of urany1 pentagonal bipyramids that are topologically identical, although compositionally distinct, to those in compreignacite. Compreignacite crystals placed in 100 ppm CsCl solution also incorporated substantial Cs by ion exchange. Ion exchange. Experiments, using Cs-exchanged compreignacite from earlier Cs by ion exchange. Ion exchange experiments, using Cs-exchanged compreignacite from earlier, in 2 M KCl solution at 90 deg for 14 days showed that compreignacite will retain significant Cs in the presence of a solution rich in K. These experiments indicate that formation of compreignacite structure-type phases in a geological repository due to alteration of nuclear waste may significantly impact upon the mobility of Cs, either by direct direct incorporation of Cs into growing crystals, or by exchange of Cs into earlier-formed crystals of compreignacite when they contact Cs-bearing solutions.