Natural analogue evidence for controls on radionuclide uptake by fractured crystalline rock

Metcalfe, Richard; Milodowski, Antoni E.; Field, Lorraine P.; Wogelius, Roy A.; Carpenter, Gráinne; Yardley, Bruce W.D.; Norris, Simon. 2021 Natural analogue evidence for controls on radionuclide uptake by fractured crystalline rock. Applied Geochemistry, 124, 104812. 10.1016/j.apgeochem.2020.104812

Before downloading, please read NORA policies.

Preview

Text (Open Access Paper)
1-s2.0-S0883292720303048-main.pdf - Published Version
Available under License Creative Commons Attribution 4.0.
Download (8MB) | Preview

Official URL: http://dx.doi.org/10.1016/j.apgeochem.2020.104812

Abstract/Summary

Fractured Crystalline Rocks (FCR) are being considered in several countries as hosts for radioactive waste repositories. In FCR, radionuclides may be transported relatively rapidly by bulk groundwater flow through open fractures, but much more slowly by diffusion through porewater in the rock matrices. Rock matrix diffusion (RMD) is the diffusion of radionuclides in the aqueous phase, between open fractures and rock matrices. Sorption or co-precipitation on the fracture surfaces and walls of the matrix pores causes further radionuclide retardation. RMD may be important in a repository's safety case and has been investigated by many published short-term (to a few years) laboratory and in-situ experiments. To improve understanding over longer timescales, we investigated evidence for RMD of several natural radioelements, and radioelement analogues, in five exemplar fractured crystalline rock (FCR) samples aged between c. 70 Ma and c. 455 Ma. The sample suite consisted of two samples of Borrowdale Volcanic Group (BVG) meta-tuff from northwest England, a sample of Carnmenellis Granite from southwest England and two samples of Toki Granite from central Japan. Uptake or loss of the studied elements is limited to an altered damage zone in each sample, coupled to mineral alteration processes. These zones are most extensive (a few tens of millimetres) in the Toki Granite samples. We also found unstable primary igneous minerals to persist in the immediate wallrocks of fractures in studied granite samples, suggesting that pores were not permanently water saturated in these samples. Although only a small sample suite was studied, the results show that while RMD may be important in some kinds of FCR, in others it may be negligible. Site-specific information is therefore needed to determine how much reliance can be placed on RMD when developing a safety case.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/j.apgeochem.2020.104812
ISSN:	08832927
Date made live:	17 Feb 2021 16:07 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/529680

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/j.apgeochem.2020.104812

ISSN:

08832927

Date made live:

17 Feb 2021 16:07 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/529680