Effect of wind turbulence on gas transport in porous media: experimental method and preliminary results
dc.contributor.author | Wilkinson, Stephen | |
dc.contributor.author | Pourbakhtiar, Alireza | |
dc.contributor.author | Poulsen, Tjalfe | |
dc.contributor.author | Bridge, Jonathan | |
dc.date.accessioned | 2017-01-19T15:29:26Z | |
dc.date.available | 2017-01-19T15:29:26Z | |
dc.date.issued | 2017-01-19 | |
dc.identifier.citation | Pourbakhtiar, A., Poulsen, T. G., Wilkinson, S. and Bridge, J. W. (2017), Effect of wind turbulence on gas transport in porous media: experimental method and preliminary results. European Journal of Soil Science, 68: 48–56. doi:10.1111/ejss.12403 | |
dc.identifier.issn | 1365-2389 | |
dc.identifier.doi | 10.1111/ejss.12403 | |
dc.identifier.uri | http://hdl.handle.net/2436/620343 | |
dc.description.abstract | Summary We demonstrate a novel experimental arrangement for measuring wind turbulence-induced gas transport in dry porous media under controlled conditions. This equipment was applied to assess the effect of wind turbulence on gas transport (quantified as a dispersion coefficient) as a function of distance to the surface of the porous medium exposed to wind. Two different strategies for the measurement of wind-induced gas transport were compared. Experiments were carried out with O2 and CO2 as tracer gases with average vertical wind speeds of 0.02–1.06ms−1. Oxygen breakthrough curves as a function of distance to the wind-exposed surface of the porous medium were analysed numerically with a finite-difference-based model to assess gas transport. We showed that wind turbulence-induced gas transport is an important transport mechanism that can be 20–70 times larger than molecular diffusion-induced transport. Wind conditions and properties of the porous medium had strong controlling effects on this relationship. Importantly, we show that even though wind-induced gas transport is greatest near to the wind-exposed surface, it can have marked effects on the variation in gas concentration at much greater depths. | |
dc.language.iso | en | |
dc.publisher | Wiley | |
dc.relation.url | http://onlinelibrary.wiley.com/doi/10.1111/ejss.12403/full | |
dc.subject | atmospheric wind turbulence | |
dc.subject | gas transport in porous media | |
dc.subject | wind-induced dispersion | |
dc.title | Effect of wind turbulence on gas transport in porous media: experimental method and preliminary results | |
dc.type | Journal article | |
dc.identifier.journal | European Journal of Soil Science | |
dc.date.accepted | 2016-11-09 | |
rioxxterms.funder | University of Wolverhampton | |
rioxxterms.identifier.project | UoW190117SW | |
rioxxterms.version | VoR | |
rioxxterms.licenseref.uri | https://creativecommons.org/CC BY-NC-ND 4.0 | |
rioxxterms.licenseref.startdate | 2017-01-19 | |
dc.source.volume | 68 | |
dc.source.issue | 1 | |
dc.source.beginpage | 48 | |
dc.source.endpage | 56 | |
refterms.dateFCD | 2018-10-19T09:23:24Z | |
refterms.versionFCD | VoR | |
refterms.dateFOA | 2017-01-19T00:00:00Z | |
html.description.abstract | Summary We demonstrate a novel experimental arrangement for measuring wind turbulence-induced gas transport in dry porous media under controlled conditions. This equipment was applied to assess the effect of wind turbulence on gas transport (quantified as a dispersion coefficient) as a function of distance to the surface of the porous medium exposed to wind. Two different strategies for the measurement of wind-induced gas transport were compared. Experiments were carried out with O2 and CO2 as tracer gases with average vertical wind speeds of 0.02–1.06ms−1. Oxygen breakthrough curves as a function of distance to the wind-exposed surface of the porous medium were analysed numerically with a finite-difference-based model to assess gas transport. We showed that wind turbulence-induced gas transport is an important transport mechanism that can be 20–70 times larger than molecular diffusion-induced transport. Wind conditions and properties of the porous medium had strong controlling effects on this relationship. Importantly, we show that even though wind-induced gas transport is greatest near to the wind-exposed surface, it can have marked effects on the variation in gas concentration at much greater depths. |