2014
DOI: 10.1007/s12665-014-3168-y
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Using field analogue soil column experiments to quantify radon-222 gas migration and transport through soils and bedrock of Halifax, Nova Scotia, Canada

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Cited by 4 publications
(2 citation statements)
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“…Hydrogen is expected to be the dominant gas generated in a deep geological repository [132,133] and could also potentially act as a carrier for radioactive gaseous species (e.g., H-3, C-14, Rn-222, etc. [134,135]). The formation of H 2 by anaerobic corrosion of metals may further contribute to gas generation (such as CH 4 , H 2 S or CO 2 ), as H 2 can be used as an electron donor in microbial processes [136].…”
Section: Effect Of Oxygen Gasses and Nutrients On The Microorganismsmentioning
confidence: 99%
“…Hydrogen is expected to be the dominant gas generated in a deep geological repository [132,133] and could also potentially act as a carrier for radioactive gaseous species (e.g., H-3, C-14, Rn-222, etc. [134,135]). The formation of H 2 by anaerobic corrosion of metals may further contribute to gas generation (such as CH 4 , H 2 S or CO 2 ), as H 2 can be used as an electron donor in microbial processes [136].…”
Section: Effect Of Oxygen Gasses and Nutrients On The Microorganismsmentioning
confidence: 99%
“…Thus, once gases are produced, environmental factors, which control the cave atmosphere, determine the gaseous accumulation in the confined atmosphere. The porous system of the rocks and soils and the presence of water define the diffusion rates of both gases [22][23][24][25]. Diffusion is among the mechanisms responsible for gas migration and accumulation in an underground environment, and it directly depends on the physical properties of the porous materials [26][27][28].…”
Section: Introductionmentioning
confidence: 99%