Abstract

In a deep geological repository (DGR) for the long-term disposal of radioactive waste, gases (e.g., hydrogen (H2), carbon dioxide (CO2) and methane (CH4)) can be generated through a number of processes, such as corrosion of various metals and alloys and degradation of organic materials. If gas induced pressure exceeds the containment capacity of the engineered barrier systems (EBS) or the host rock, the gases could migrate through these barriers and potentially expose people and the environment to radiation. Therefore, a good understanding on the long-term performance of these barriers against gas migration is an important component in DGR design and safety assessment. In the present work, a numerical model has been developed to simulate the diffusion of CO2 (one of the gas species) in the near field of a DGR with the generation from related chemical reactions. The generation of CO2 was investigated to determine if it is a critical factor to impact the DGR safety under Canadian geological formations. A commercial computational fluid dynamics (CFD) code, ANSYS Fluent was used for the calculations. The model considered pH and temperature effects on CO2 migration under Canadian DGR geochemistry conditions.

References

1.
Leupin
,
O. X.
,
Zeyer
,
J.
,
Cloet
,
V.
,
Smith
,
P.
,
Bernier Latmani
,
R.
,
Marschall
,
P.
,
Papafotiou
,
A.
,
Schwyn
,
B.
, and
Stroes Gascoyne
,
S.
,
2016
, “
An Assessment of the Possible Fate of Gas Generated in a Repository for Low and Intermediate Level Waste
,”
National Cooperative for the Disposal of Radioactive Waste (NAGRA)
,
Switzerland
, Report No.
NTB--16-05.
2.
Dagher
,
E. E.
,
Nguyen
,
T. S.
, and
Sedano
,
J. A. I.
,
2019
, “
Development of a Mathematical Model for Gas Migration (Two Phase Flow) in Natural and Engineered Barriers for Radioactive Waste Disposal
,” Multiple Roles of Clays in Radioactive Waste Confinement,
Geological Society
, Special Publications 482,
London
, UK, pp.
115
148
.10.1144/SP482.14
3.
ANSYS Fluent
,
2020
, “
R2 Documentation
,” ANSYS Inc., Canonsburg, PA, accessed Nov. 20, 2024, https://www.ansys.com/products/fluids/ansys-fluent
4.
Birkholzer
,
J. T.
,
Tsang
,
C.
,
Bond
,
A. E.
,
Hudson
,
J. A.
,
Jing
,
L.
, and
Stephansson
,
O.
,
2019
, “
25 Years of DECOVALEX Scientific Advances and Lessons Learned From an International Research Collaboration in Coupled Subsurface Processes
,”
Int. J. Rock Mech. Min. Sci.
,
122
, p.
103995
.10.1016/j.ijrmms.2019.03.015
5.
Shaw
,
R. P.
,
2015
, “
The Fate of Repository Gases (FORGE) Project
,”
Gas Generation and Migration in Deep Geological Radioactive Waste Repositories
,
Geological Society, Special Publications 415
,
London
, pp.
1
7
.
6.
Calder
,
N.
,
Avis
,
J.
,
Humphreys
,
P.
,
King
,
F.
,
Suckling
,
P.
, and
Walsh
,
R.
,
2009
, “
Postclosure Safety Assessment: Gas Modelling
,”
NWMO
,
Toronto, Canada
, Report No.
DGR-TR-2009-07.
7.
Saâdi
,
Z.
,
2024
, “
Gas-Entry Pressure Impact on the Evaluation of Hydrogen Migration at Different Scales of a Deep Geological Disposal of Radioactive Waste
,”
Sci. Rep.
,
14
(
1
), p.
6221
.10.1038/s41598-024-56454-y
8.
Hou
,
S. X.
,
Maitland
,
G. C.
, and
Trusler
,
M. C.
,
2013
, “
Measurement and Modeling of the Phase Behaviour of the (Carbon Dioxide + Water) Mixture at Temperatures From 298.15 to 448.15 K
,”
J. Supercrit. Fluids
,
73
, pp.
87
96
.10.1016/j.supflu.2012.11.011
9.
Mohammadian
,
E.
,
Hamidi
,
H.
,
Asadullah
,
M.
,
Azdarpour
,
A.
,
Motamedi
,
S.
, and
Junin
,
R.
,
2015
, “
Measurement of CO2 Solubility in NaCl Brine Solutions at Different Temperatures and Pressures Using the Potentiometric Titration Method
,”
J. Chem. Eng. Data
,
60
(
7
), pp.
2042
2049
.10.1021/je501172d
10.
Wang
,
P.
, and
Anderko
,
A.
,
2011
, “
Modeling Chemical Equilibria, Phase Behavior, and Transport Properties in Ionic Liquid Systems
,”
Fluid Phase Equilib.
,
302
(
1–2
), pp.
74
82
.10.1016/j.fluid.2010.08.011
11.
Xu
,
T.
,
Senger
,
R.
, and
Finsterle
,
S.
,
2008
, “
Corrosion Induced Gas Generation in a Nuclear Waste Repository: Reactive Geochemistry and Multiphase Flow Effects
,”
Appl. Geochem.
,
23
(
12
), pp.
3423
3433
.10.1016/j.apgeochem.2008.07.012
12.
Perera
,
P. N.
,
Deng
,
H.
,
Schuck
,
P. J.
, and
Gilbert
,
B.
,
2018
, “
Diffusivity of Carbon Dioxide in Aqueous Solutions Under Geologic Carbon Sequestration Conditions
,”
J. Phys. Chem. B
,
122
(
16
), pp.
4566
4572
.10.1021/acs.jpcb.8b00802
13.
Cadogan
,
S. P.
,
Maitland
,
G. C.
, and
Trusler
,
J. P. M.
,
2014
, “
Diffusion Coefficients of CO2 and N2 in Water at Temperatures Between 298.15 K and 423.15 K at Pressures Up to 45 MPa
,”
J. Chem. Eng. Data
,
59
(
2
), pp.
519
525
.10.1021/je401008s
14.
Walke
,
R.
,
Humphreys
,
P.
,
King
,
F.
,
Little
,
R.
,
Metcalfe
,
R.
,
Penfold
,
J.
,
Towler
,
G.
,
Walsh
,
R.
, and
Wilson
,
J.
,
2011
, “
Postclosure Safety Assessment: Data
,”
Nuclear Waste Management Organization (NWMO)
,
Toronto, Canada
, Report No.
DGR-TR-2011-32.
15.
Qiu
,
L.
, and
Qian
,
J.
,
2023
, “
Calcite Dissolution and CO2 Generation Under Deep Geological Conditions
,”
5th Canadian Conference on Waste Management, Decommissioning and Environmental Restoration
,
Niagara Falls, ON, Canada
, Aug.
27
31
.
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