E. Conley et J. Genin, NUCLEAR WASTE STORAGE VAULT CLOSURE DETERMINATION, Radioactive waste management and the nuclear fuel cycle, 17(3-4), 1993, pp. 177-194
Engineers have little experience burying nuclear waste deep in 280 mil
lion-year-old salt deposits. We know that storage vaults, carved from
the salt, close in on themselves and that waste placed therein will ev
entually be encapsulated. We do not know, however, how much time this
process will require. Nor do we know the extent that temperature varia
tions, moisture or faults evident in the walls, will affect the waste
barrels or their contents. If underground, long-term nuclear waste dis
posal is to become widely accepted, behavior of the disturbed salt bed
s must be reasonably predictable. At present, the deformation mechanis
m is not fully understood; the research we have undertaken addresses t
his question. In particular, a comprehensive mathematical model and co
mputer algorithm is being developed to predict the action of the encap
sulating mechanism. Equally important, the model is being experimental
ly validated in situ at the Waste Isolation Pilot Plant (WIPP) site in
Carlsbad, NM. Two parallel and related, but also distinct research ef
forts are now united. In addition to the modeling effort, experiments
are being performed at the WIPP site to obtain precise values for crit
ical model parameters. The simultaneous development of an analytical m
odel together with comprehensive determination of the requisite bounda
ry conditions and material and structural properties will yield an acc
urate working model of salt closure. The progress to date is detailed.