16–21 Sept 2012
Como, Italy
Europe/Rome timezone

Generation of inorganic colloids in the chemical disturbed zone in the proximity of a cementitious repository

19 Sept 2012, 18:00
1h 50m
Como, Italy

Como, Italy

Grand Hotel di Como Via per Cernobbio 41A 22100 Como, Italy
Poster Radioactive elements in the environment, radiation archeometry and Health Physics Poster Session

Speaker

Dr Monica Felipe-Sotelo (Loughborough University, UK)

Description

The current concept for the disposal of intermediate- and low-level waste in the UK involves the placement of grouted waste confined in stainless steel canisters in a cementitious repository deep underground. While the cement will buffer the porewater to a highly alkaline pH, contributing to the retardation of radionuclides by precipitation, this could potentially create an alkaline plume moving from the repository into the host rock. The alkaline cement leachate can react with the host rock, promoting dissolution of some mineral phases, precipitation of new phases and the generation of colloids that may affect radionuclide movement within the chemically disturbed zone of the host rock. The aim of the present work is to study the generation of inorganic colloids from a generic host rock in contact with an alkaline plume. An intact core of sandstone has had an artificial “young” cement leachate (pH 13.10) under CO2-free conditions pumped through it. The solution at the outlet was then sequentially ultrafiltered in-line through a rig fitted with 12 µm, 1 µm, 30 kDa and 1 kDa membranes. After passing more than 500 pore volumes of the young cement leachate, the imaging of the filters by Scanning Electron Microscopy (SEM) in combination with X-ray microanalysis showed no evidence of the formation of inorganic colloids under these experimental conditions. On the other hand, analysis of the outlet solution by ICP-MS indicates that there is significant dissolution of some mineral phases present in the sandstone, however no difference were found between the elemental composition of the solution before and after ultrafiltration. Additional tests with artificial colloids indicate that silica and iron oxides colloids are unstable in “young” cement leachate. Acknowledgments: The authors would like to thank NERC for the funding of the BIGRAD consortium.

Primary author

Dr Monica Felipe-Sotelo (Loughborough University, UK)

Co-authors

Dr Antoni Milodowski (British Geological Survey) Dr Nick Bryan (The University of Manchester) Nick Evans (Loughborough University)

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