Dry deposition of particles to wave surfaces: I. Mathematical modeling
Previous estimates of dry deposition to water surfaces were generally based on deposition to flat, solid surfaces. This paper examines the effects of waves on dry deposition rates by numerically simulating particle trajectories over wave surfaces. Airflows over two-dimensional sine waves with height...
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Veröffentlicht in: | Atmospheric environment (1994) 1999-11, Vol.33 (26), p.4273-4281 |
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creator | Zufall, Maria J. Dai, Weiping Davidson, Cliff I. Etyemezian, Vicken |
description | Previous estimates of dry deposition to water surfaces were generally based on deposition to flat, solid surfaces. This paper examines the effects of waves on dry deposition rates by numerically simulating particle trajectories over wave surfaces. Airflows over two-dimensional sine waves with height-to-length ratios 2
a/
λ=0.1, 0.07, and 0.03 were calculated with a commercial computational fluid dynamics model. Results from the airflow simulations (velocity, kinetic energy, energy dissipation rate, and shear stress) provided inputs for a stochastic particle trajectory model. Particles were released from a height of 300 non-dimensional wall units at different locations along the wave. For those between 1 and 20
μm, deposition was found to be greatest for particles released to the upslope portion of the wave, followed by the trough, crest and downslope. Overall deposition rates were enhanced due to the presence of waves. Increases ranged from 5% (
d
p=80
μm) to 100% (
d
p=1
μm) for waves with 2
a/
λ=0.07 and 0.1 and were approximately 50% greater (
d
p=1−80
μm) for 2
a/
λ=0.03. Deposition rates were enhanced due to increases in impaction and turbulent transport, both of which increase with increasing wave slope. However, an increased slope also produced regions of low or reversed flow in the trough and downslope, which decreased deposition rates. Due to these competing effects with respect to wave slope, deposition rates did not increase monotonically with wave slope. |
doi_str_mv | 10.1016/S1352-2310(99)00177-6 |
format | Article |
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a/
λ=0.1, 0.07, and 0.03 were calculated with a commercial computational fluid dynamics model. Results from the airflow simulations (velocity, kinetic energy, energy dissipation rate, and shear stress) provided inputs for a stochastic particle trajectory model. Particles were released from a height of 300 non-dimensional wall units at different locations along the wave. For those between 1 and 20
μm, deposition was found to be greatest for particles released to the upslope portion of the wave, followed by the trough, crest and downslope. Overall deposition rates were enhanced due to the presence of waves. Increases ranged from 5% (
d
p=80
μm) to 100% (
d
p=1
μm) for waves with 2
a/
λ=0.07 and 0.1 and were approximately 50% greater (
d
p=1−80
μm) for 2
a/
λ=0.03. Deposition rates were enhanced due to increases in impaction and turbulent transport, both of which increase with increasing wave slope. However, an increased slope also produced regions of low or reversed flow in the trough and downslope, which decreased deposition rates. Due to these competing effects with respect to wave slope, deposition rates did not increase monotonically with wave slope.</description><identifier>ISSN: 1352-2310</identifier><identifier>EISSN: 1873-2844</identifier><identifier>DOI: 10.1016/S1352-2310(99)00177-6</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Applied sciences ; Atmospheric pollution ; Continental surface waters ; Dry deposition flux ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Lake Michigan ; Meteorology ; Natural water pollution ; Particle trajectory ; Particles and aerosols ; Pollutants physicochemistry study: properties, effects, reactions, transport and distribution ; Pollution ; Turbulence ; Water treatment and pollution ; Wave slope</subject><ispartof>Atmospheric environment (1994), 1999-11, Vol.33 (26), p.4273-4281</ispartof><rights>1999 Elsevier Science Ltd</rights><rights>1999 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c464t-ab21237243c56f4c4b989e60cab7d55dfc9c7b5403aa1fbc298aebffd9da8eb03</citedby><cites>FETCH-LOGICAL-c464t-ab21237243c56f4c4b989e60cab7d55dfc9c7b5403aa1fbc298aebffd9da8eb03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/S1352-2310(99)00177-6$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,778,782,3539,27907,27908,45978</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1949348$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Zufall, Maria J.</creatorcontrib><creatorcontrib>Dai, Weiping</creatorcontrib><creatorcontrib>Davidson, Cliff I.</creatorcontrib><creatorcontrib>Etyemezian, Vicken</creatorcontrib><title>Dry deposition of particles to wave surfaces: I. Mathematical modeling</title><title>Atmospheric environment (1994)</title><description>Previous estimates of dry deposition to water surfaces were generally based on deposition to flat, solid surfaces. This paper examines the effects of waves on dry deposition rates by numerically simulating particle trajectories over wave surfaces. Airflows over two-dimensional sine waves with height-to-length ratios 2
a/
λ=0.1, 0.07, and 0.03 were calculated with a commercial computational fluid dynamics model. Results from the airflow simulations (velocity, kinetic energy, energy dissipation rate, and shear stress) provided inputs for a stochastic particle trajectory model. Particles were released from a height of 300 non-dimensional wall units at different locations along the wave. For those between 1 and 20
μm, deposition was found to be greatest for particles released to the upslope portion of the wave, followed by the trough, crest and downslope. Overall deposition rates were enhanced due to the presence of waves. Increases ranged from 5% (
d
p=80
μm) to 100% (
d
p=1
μm) for waves with 2
a/
λ=0.07 and 0.1 and were approximately 50% greater (
d
p=1−80
μm) for 2
a/
λ=0.03. Deposition rates were enhanced due to increases in impaction and turbulent transport, both of which increase with increasing wave slope. However, an increased slope also produced regions of low or reversed flow in the trough and downslope, which decreased deposition rates. Due to these competing effects with respect to wave slope, deposition rates did not increase monotonically with wave slope.</description><subject>Applied sciences</subject><subject>Atmospheric pollution</subject><subject>Continental surface waters</subject><subject>Dry deposition flux</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Lake Michigan</subject><subject>Meteorology</subject><subject>Natural water pollution</subject><subject>Particle trajectory</subject><subject>Particles and aerosols</subject><subject>Pollutants physicochemistry study: properties, effects, reactions, transport and distribution</subject><subject>Pollution</subject><subject>Turbulence</subject><subject>Water treatment and pollution</subject><subject>Wave slope</subject><issn>1352-2310</issn><issn>1873-2844</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqFkEtLxDAUhYso-PwJQhYiuqjm2TRuRHwOKC7UdbhNbzTSacakM-K_tzqKS1f3Lr5zDnxFscvoEaOsOn5gQvGSC0YPjDmklGldVivFBqu1KHkt5er4_yLrxWbOr5RSoY3eKK4u0gdpcRZzGELsSfRkBmkIrsNMhkjeYYEkz5MHh_mETI7IHQwvOIURgY5MY4td6J-3izUPXcadn7tVPF1dPp7flLf315Pzs9vSyUoOJTSccaG5FE5VXjrZmNpgRR00ulWq9c443ShJBQDzjeOmBmy8b00LNTZUbBX7y95Zim9zzIOdhuyw66DHOM-W1apSWvL_Qal4JQwbQbUEXYo5J_R2lsIU0odl1H7ptd967Zc7a4z91murMbf3MwB5NOET9C7kv7CRRsh6xE6XGI5WFgGTzS5g77ANCd1g2xj-GfoEuluO3w</recordid><startdate>19991101</startdate><enddate>19991101</enddate><creator>Zufall, Maria J.</creator><creator>Dai, Weiping</creator><creator>Davidson, Cliff I.</creator><creator>Etyemezian, Vicken</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>C1K</scope><scope>SOI</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>19991101</creationdate><title>Dry deposition of particles to wave surfaces: I. Mathematical modeling</title><author>Zufall, Maria J. ; Dai, Weiping ; Davidson, Cliff I. ; Etyemezian, Vicken</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c464t-ab21237243c56f4c4b989e60cab7d55dfc9c7b5403aa1fbc298aebffd9da8eb03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>Applied sciences</topic><topic>Atmospheric pollution</topic><topic>Continental surface waters</topic><topic>Dry deposition flux</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Lake Michigan</topic><topic>Meteorology</topic><topic>Natural water pollution</topic><topic>Particle trajectory</topic><topic>Particles and aerosols</topic><topic>Pollutants physicochemistry study: properties, effects, reactions, transport and distribution</topic><topic>Pollution</topic><topic>Turbulence</topic><topic>Water treatment and pollution</topic><topic>Wave slope</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zufall, Maria J.</creatorcontrib><creatorcontrib>Dai, Weiping</creatorcontrib><creatorcontrib>Davidson, Cliff I.</creatorcontrib><creatorcontrib>Etyemezian, Vicken</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Environment Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Atmospheric environment (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zufall, Maria J.</au><au>Dai, Weiping</au><au>Davidson, Cliff I.</au><au>Etyemezian, Vicken</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dry deposition of particles to wave surfaces: I. Mathematical modeling</atitle><jtitle>Atmospheric environment (1994)</jtitle><date>1999-11-01</date><risdate>1999</risdate><volume>33</volume><issue>26</issue><spage>4273</spage><epage>4281</epage><pages>4273-4281</pages><issn>1352-2310</issn><eissn>1873-2844</eissn><abstract>Previous estimates of dry deposition to water surfaces were generally based on deposition to flat, solid surfaces. This paper examines the effects of waves on dry deposition rates by numerically simulating particle trajectories over wave surfaces. Airflows over two-dimensional sine waves with height-to-length ratios 2
a/
λ=0.1, 0.07, and 0.03 were calculated with a commercial computational fluid dynamics model. Results from the airflow simulations (velocity, kinetic energy, energy dissipation rate, and shear stress) provided inputs for a stochastic particle trajectory model. Particles were released from a height of 300 non-dimensional wall units at different locations along the wave. For those between 1 and 20
μm, deposition was found to be greatest for particles released to the upslope portion of the wave, followed by the trough, crest and downslope. Overall deposition rates were enhanced due to the presence of waves. Increases ranged from 5% (
d
p=80
μm) to 100% (
d
p=1
μm) for waves with 2
a/
λ=0.07 and 0.1 and were approximately 50% greater (
d
p=1−80
μm) for 2
a/
λ=0.03. Deposition rates were enhanced due to increases in impaction and turbulent transport, both of which increase with increasing wave slope. However, an increased slope also produced regions of low or reversed flow in the trough and downslope, which decreased deposition rates. Due to these competing effects with respect to wave slope, deposition rates did not increase monotonically with wave slope.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/S1352-2310(99)00177-6</doi><tpages>9</tpages></addata></record> |
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subjects | Applied sciences Atmospheric pollution Continental surface waters Dry deposition flux Earth, ocean, space Exact sciences and technology External geophysics Lake Michigan Meteorology Natural water pollution Particle trajectory Particles and aerosols Pollutants physicochemistry study: properties, effects, reactions, transport and distribution Pollution Turbulence Water treatment and pollution Wave slope |
title | Dry deposition of particles to wave surfaces: I. Mathematical modeling |
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