dc.contributor.author | Fossum, Hannibal Eie | |
dc.contributor.author | Reif, Bjørn Anders Pettersson | |
dc.contributor.author | Tutkun, Murat | |
dc.contributor.author | Gjesdal, Thor | |
dc.date.accessioned | 2017-10-24T06:35:11Z | |
dc.date.accessioned | 2017-10-25T10:59:58Z | |
dc.date.available | 2017-10-24T06:35:11Z | |
dc.date.available | 2017-10-25T10:59:58Z | |
dc.date.issued | 2012 | |
dc.identifier.citation | Fossum HE, Reif BAP, Tutkun M, Gjesdal T. On the Use of Computational Fluid Dynamics to Investigate Aerosol Dispersion in an Industrial Environment: A Case Study. Boundary-layer Meteorology. 2012;144(1):21-40 | en_GB |
dc.identifier.uri | http://hdl.handle.net/20.500.12242/719 | |
dc.identifier.uri | https://ffi-publikasjoner.archive.knowledgearc.net/handle/20.500.12242/719 | |
dc.description | Fossum, Hannibal Eie; Reif, Bjørn Anders Pettersson; Tutkun, Murat; Gjesdal, Thor.
On the Use of Computational Fluid Dynamics to Investigate Aerosol Dispersion in an Industrial Environment: A Case Study. Boundary-layer Meteorology 2012 ;Volum 144.(1) s. 21-40 | en_GB |
dc.description.abstract | Aerosol dispersion in the area surrounding an existing biological treatment facility is investigated using large-eddy simulation, with the objective to investigate the applicability of computational fluid dynamics to complex real-life problems. The aerosol sources consist of two large aeration ponds that slowly diffuse aerosols into the atmosphere. These sources are modelled as dilute concentrations of a non-buoyant non-reacting pollutant diffusing from two horizontal surfaces. The time frame of the aerosol release is restricted to the order of minutes, justifying a statistically steady inlet boundary condition. The numerical results are compared to wind-tunnel experiments for validation. The wind-tunnel flow characteristics resemble neutral atmospheric conditions with a Reynolds number, based on the boundary-layer thickness, of Reδ ≈ 2 × 105. The numerical inflow conditions are based upon the wind-tunnel flow field. The predicted decay of both the mean and root-mean-square concentrations are in good agreement with experimental data; at 3 m from the ground, the plume mean concentration 200 m downwind of the source is approximately 2% of the source strength. The numerical data in the near-surface layer (0–50 m from the ground) correspond particularly well with the wind-tunnel data. Tentative deposition simulations suggest that there seems to be little difference in the deposition rates of large (1.8 × 10−5 m) and small (3 × 10−6 m) particles in the near-field under the flow conditions considered. | en_GB |
dc.language.iso | en | en_GB |
dc.title | On the Use of Computational Fluid Dynamics to Investigate Aerosol Dispersion in an Industrial Environment: A Case Study | en_GB |
dc.type | Article | en_GB |
dc.date.updated | 2017-10-24T06:35:11Z | |
dc.identifier.cristinID | 952555 | |
dc.identifier.cristinID | 952555 | |
dc.identifier.doi | 10.1007/s10546-012-9711-z | |
dc.source.issn | 0006-8314 | |
dc.source.issn | 1573-1472 | |
dc.type.document | Journal article | |
dc.relation.journal | Boundary-layer Meteorology | |