Description
Transport of radionuclides will most likely take place through the intact matrix, both upwards and downwards to local/regional aquifers. Transport in natural and / or repository-induced inhomogeneities is unlikely because of the efficient self-sealing capacity of the Opalinus Clay.
OPA Category
Category as used in the OPA assessment
OPA host rock
OPA Number
Number as used in the OPA assessment
3.01
NEA V1 IFEP Reference(s)
Related IFEPs from the NEA V1 IFEP list from 1999
2.2.07, 3.2.07, 2.2.05, 2.2.03