Description
Oxidising porewater may have an adverse effect on the retention of some radionuclides. In their oxidised form radionuclides may be better soluble and have lower sorption constants (examples: U, Tc). The pyrite in the host rock may be oxidised leading to higher sulphate concentrations in the porewater. The pH value may also decrease but Opalinus Clay is well buffered by its calcite content. The low hydraulic conductivity of Opalinus Clay and the strong buffering by pyrite and organic matter prevent oxidising water from entering from overlying or underlying rocks.
OPA Category
Category as used in the OPA assessment
OPA host rock
OPA Number
Number as used in the OPA assessment
4.03
NEA V1 IFEP Reference(s)
Related IFEPs from the NEA V1 IFEP list from 1999
2.2.08, 3.2.02, 3.2.03