Estimating aggregation between suspended sediments and frazil ice
Abstract. This paper aims to describe the scavenging pro-cess, one of the main processes for incorporating sediments (particles) into sea ice. An experiment with suspended sed-iment and frazil ice in a homogeneous turbulent flow is pre-sented. At the end sediment where incorporated into the surface...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.568.9881 2023-05-15T18:18:19+02:00 Estimating aggregation between suspended sediments and frazil ice Lars H. Smedsrud The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.9881 http://folk.uib.no/ngfls/mypapers/smedsrud98.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.9881 http://folk.uib.no/ngfls/mypapers/smedsrud98.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://folk.uib.no/ngfls/mypapers/smedsrud98.pdf text ftciteseerx 2016-01-08T12:24:01Z Abstract. This paper aims to describe the scavenging pro-cess, one of the main processes for incorporating sediments (particles) into sea ice. An experiment with suspended sed-iment and frazil ice in a homogeneous turbulent flow is pre-sented. At the end sediment where incorporated into the surface grease ice. The ice production was constant, and calculated from the salinity measurements, while the tur-bulent dissipation rate was calculated from high resolution current measurements. A model for aggregation between suspended sediment and frazil is also presented and used to simulate the experi-ment. The modelled aggregation process depends primarily on concentrations, on the turbulence levels, and on the (con-stant) radii of the sediments and ice. Eciency of the aggregation process is estimated from the model and experimental results, and the "aggregation" factor is found to be 0.025. This is consistent with the-oretical estimates, qualitative observations from laboratory experiments, and eld data. Sensitivity analyses suggest that the results does not depend greatly on uncertainty of model parameters. Text Sea ice Unknown |
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description |
Abstract. This paper aims to describe the scavenging pro-cess, one of the main processes for incorporating sediments (particles) into sea ice. An experiment with suspended sed-iment and frazil ice in a homogeneous turbulent flow is pre-sented. At the end sediment where incorporated into the surface grease ice. The ice production was constant, and calculated from the salinity measurements, while the tur-bulent dissipation rate was calculated from high resolution current measurements. A model for aggregation between suspended sediment and frazil is also presented and used to simulate the experi-ment. The modelled aggregation process depends primarily on concentrations, on the turbulence levels, and on the (con-stant) radii of the sediments and ice. Eciency of the aggregation process is estimated from the model and experimental results, and the "aggregation" factor is found to be 0.025. This is consistent with the-oretical estimates, qualitative observations from laboratory experiments, and eld data. Sensitivity analyses suggest that the results does not depend greatly on uncertainty of model parameters. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
author |
Lars H. Smedsrud |
spellingShingle |
Lars H. Smedsrud Estimating aggregation between suspended sediments and frazil ice |
author_facet |
Lars H. Smedsrud |
author_sort |
Lars H. Smedsrud |
title |
Estimating aggregation between suspended sediments and frazil ice |
title_short |
Estimating aggregation between suspended sediments and frazil ice |
title_full |
Estimating aggregation between suspended sediments and frazil ice |
title_fullStr |
Estimating aggregation between suspended sediments and frazil ice |
title_full_unstemmed |
Estimating aggregation between suspended sediments and frazil ice |
title_sort |
estimating aggregation between suspended sediments and frazil ice |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.9881 http://folk.uib.no/ngfls/mypapers/smedsrud98.pdf |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
http://folk.uib.no/ngfls/mypapers/smedsrud98.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.9881 http://folk.uib.no/ngfls/mypapers/smedsrud98.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766194861944340480 |