2021
DOI: 10.3390/su131810007
|View full text |Cite
|
Sign up to set email alerts
|

Diffusive Transport of Dissolved Gases in Potential Concretes for Nuclear Waste Disposal

Abstract: In many countries, the preferred option for the long-term management of high- and intermediate level radioactive waste and spent fuel is final disposal in a geological repository. In this geological repository, the generation of gas will be unavoidable. In order to make a correct balance between gas generation and dissipation by diffusion, knowledge of the diffusion coefficients of gases in the host rock and the engineered barriers is essential. Currently, diffusion coefficients for the Boom Clay, a potential … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
4
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
8
1
1

Relationship

2
8

Authors

Journals

citations
Cited by 13 publications
(5 citation statements)
references
References 25 publications
0
4
0
Order By: Relevance
“…Gas pressure build-up due to H 2 release might lead to gas migration in the geotechnical and geological barrier [23]. In the initially partially liquid saturated repository where a distinct gaseous phase is present, gas migration will likely occur via advection whereas in the fully liquid saturated host rock (and after the re-saturation of the backfilled repository, in the saturated bentonite), dissolved gas will be transported diffusively, driven by dissolved gas concentration gradients [18,29]. The transport of gas, be it by diffusion or advection in the liquid or gaseous phase, can imply the transport of radio nuclides [30].…”
Section: Relevant Thm-coupled Processes In Hlw Repositoriesmentioning
confidence: 99%
“…Gas pressure build-up due to H 2 release might lead to gas migration in the geotechnical and geological barrier [23]. In the initially partially liquid saturated repository where a distinct gaseous phase is present, gas migration will likely occur via advection whereas in the fully liquid saturated host rock (and after the re-saturation of the backfilled repository, in the saturated bentonite), dissolved gas will be transported diffusively, driven by dissolved gas concentration gradients [18,29]. The transport of gas, be it by diffusion or advection in the liquid or gaseous phase, can imply the transport of radio nuclides [30].…”
Section: Relevant Thm-coupled Processes In Hlw Repositoriesmentioning
confidence: 99%
“…The experimental setup for measuring permeability is the same as the one used on a similar sandy clay sample in a previous study [17]. This setup has not been modified because it is highly reliable and has been used to make K measurements for different samples [17]. Hydraulic conductivities are generally measured by imposing constant pressure gradients across the faces of the sample.…”
Section: Water Permeability Measurementsmentioning
confidence: 99%
“…The diffusion coefficients of initial materials were determined before and after a given time of interaction, similar to permeability. As presented in (Jacops et al 2021), a through-diffusion methodology was used to determine the diffusivities of two dissolved gases (He and CH4) in a single experiment. It is worth noting that the permeability/percolation cell can be readily detached and then rejoined to the diffusion setup due to its compatibility.…”
Section: Diffusivitymentioning
confidence: 99%