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Experimental research on dust lifting by propagating shock wave
The aim of the presented work was to study the dust lifting process from a layer of dust behind a propagating shock wave. The experiments were conducted with the use of a shock tube and a specially constructed, five-channel laser optical device enabling measurements at five positions located in one...
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Published in: | Shock waves 2017-03, Vol.27 (2), p.179-186 |
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description | The aim of the presented work was to study the dust lifting process from a layer of dust behind a propagating shock wave. The experiments were conducted with the use of a shock tube and a specially constructed, five-channel laser optical device enabling measurements at five positions located in one vertical plane along the height of the tube. The system enabled measurements of the delay in lifting up of the dust from the layer, and the vertical velocity of the dust cloud was calculated from the dust concentration measurements. The research was carried out for various initial conditions and for three fractions of black coal dust. In the presented tests, three shock wave velocities: 450, 490 and 518 m/s and three dust layer thicknesses, equal to 1.0, 1.5 and 2.0 mm, were taken into consideration. On the grounds of the obtained experimental results, it was assumed that the vertical component of the lifted dust velocity is a function of the dust particle diameter, the velocity of the air flow in the channel, the layer thickness and the dust bulk density. It appeared, however, that lifting up of the dust from the thick layers, thicker than 1 mm, is a more complex process than that from thin layers and still requires further research. A possible explanation is that the shock wave action upon the thick layer results in its aggregation in the first stage of the dispersing process, which suppresses the dust lifting process. |
doi_str_mv | 10.1007/s00193-016-0661-0 |
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It appeared, however, that lifting up of the dust from the thick layers, thicker than 1 mm, is a more complex process than that from thin layers and still requires further research. 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The experiments were conducted with the use of a shock tube and a specially constructed, five-channel laser optical device enabling measurements at five positions located in one vertical plane along the height of the tube. The system enabled measurements of the delay in lifting up of the dust from the layer, and the vertical velocity of the dust cloud was calculated from the dust concentration measurements. The research was carried out for various initial conditions and for three fractions of black coal dust. In the presented tests, three shock wave velocities: 450, 490 and 518 m/s and three dust layer thicknesses, equal to 1.0, 1.5 and 2.0 mm, were taken into consideration. On the grounds of the obtained experimental results, it was assumed that the vertical component of the lifted dust velocity is a function of the dust particle diameter, the velocity of the air flow in the channel, the layer thickness and the dust bulk density. It appeared, however, that lifting up of the dust from the thick layers, thicker than 1 mm, is a more complex process than that from thin layers and still requires further research. A possible explanation is that the shock wave action upon the thick layer results in its aggregation in the first stage of the dispersing process, which suppresses the dust lifting process.</description><subject>Acoustics</subject><subject>Air flow</subject><subject>Bulk density</subject><subject>Coal dust</subject><subject>Condensed Matter Physics</subject><subject>Dust</subject><subject>Engineering</subject><subject>Engineering Fluid Dynamics</subject><subject>Engineering Thermodynamics</subject><subject>Fluid- and Aerodynamics</subject><subject>Heat and Mass Transfer</subject><subject>Hoisting</subject><subject>Initial conditions</subject><subject>Original Article</subject><subject>Particle size</subject><subject>Shock waves</subject><subject>Thermodynamics</subject><subject>Thickness</subject><subject>Thin films</subject><subject>Vertical orientation</subject><subject>Wave dispersion</subject><subject>Wave velocity</subject><issn>0938-1287</issn><issn>1432-2153</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp1kEtPwzAQhC0EEqXwA7hZ4mzYdWLHPiFUlYeExAXOlmM7fVCSYKdA_z0u4cCF02qlb2Z3hpBzhEsEqK4SAOqCAUoGUiKDAzLBsuCMoygOyQR0oRhyVR2Tk5TWma5kVU3I9fyrD3H1FtrBbmgMKdjolrRrqd-mgW5WzbBqF7Te0T52vV3YnzUtO_dKP-1HOCVHjd2kcPY7p-Tldv48u2ePT3cPs5tH5gqhByYaB8op1N6DUsGV0juvg1dCSuWsFqLmjQTBsQGorSzBg9Vcc1eEGnVdTMnF6JvfeN-GNJh1t41tPmlQKchhykpmCkfKxS6lGBrT52w27gyC2fdkxp5M7snsezKQNXzUpMy2ixD_OP8r-ga0Imp3</recordid><startdate>20170301</startdate><enddate>20170301</enddate><creator>Żydak, P.</creator><creator>Oleszczak, P.</creator><creator>Klemens, R.</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20170301</creationdate><title>Experimental research on dust lifting by propagating shock wave</title><author>Żydak, P. ; Oleszczak, P. ; Klemens, R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c359t-5fc08c819dd088ec46dcd9ed85668ca955b2f60521f00ba640d0a9292c3eb19b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Acoustics</topic><topic>Air flow</topic><topic>Bulk density</topic><topic>Coal dust</topic><topic>Condensed Matter Physics</topic><topic>Dust</topic><topic>Engineering</topic><topic>Engineering Fluid Dynamics</topic><topic>Engineering Thermodynamics</topic><topic>Fluid- and Aerodynamics</topic><topic>Heat and Mass Transfer</topic><topic>Hoisting</topic><topic>Initial conditions</topic><topic>Original Article</topic><topic>Particle size</topic><topic>Shock waves</topic><topic>Thermodynamics</topic><topic>Thickness</topic><topic>Thin films</topic><topic>Vertical orientation</topic><topic>Wave dispersion</topic><topic>Wave velocity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Żydak, P.</creatorcontrib><creatorcontrib>Oleszczak, P.</creatorcontrib><creatorcontrib>Klemens, R.</creatorcontrib><collection>SpringerOpen</collection><collection>CrossRef</collection><jtitle>Shock waves</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Żydak, P.</au><au>Oleszczak, P.</au><au>Klemens, R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Experimental research on dust lifting by propagating shock wave</atitle><jtitle>Shock waves</jtitle><stitle>Shock Waves</stitle><date>2017-03-01</date><risdate>2017</risdate><volume>27</volume><issue>2</issue><spage>179</spage><epage>186</epage><pages>179-186</pages><issn>0938-1287</issn><eissn>1432-2153</eissn><abstract>The aim of the presented work was to study the dust lifting process from a layer of dust behind a propagating shock wave. The experiments were conducted with the use of a shock tube and a specially constructed, five-channel laser optical device enabling measurements at five positions located in one vertical plane along the height of the tube. The system enabled measurements of the delay in lifting up of the dust from the layer, and the vertical velocity of the dust cloud was calculated from the dust concentration measurements. The research was carried out for various initial conditions and for three fractions of black coal dust. In the presented tests, three shock wave velocities: 450, 490 and 518 m/s and three dust layer thicknesses, equal to 1.0, 1.5 and 2.0 mm, were taken into consideration. On the grounds of the obtained experimental results, it was assumed that the vertical component of the lifted dust velocity is a function of the dust particle diameter, the velocity of the air flow in the channel, the layer thickness and the dust bulk density. It appeared, however, that lifting up of the dust from the thick layers, thicker than 1 mm, is a more complex process than that from thin layers and still requires further research. A possible explanation is that the shock wave action upon the thick layer results in its aggregation in the first stage of the dispersing process, which suppresses the dust lifting process.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00193-016-0661-0</doi><tpages>8</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Acoustics Air flow Bulk density Coal dust Condensed Matter Physics Dust Engineering Engineering Fluid Dynamics Engineering Thermodynamics Fluid- and Aerodynamics Heat and Mass Transfer Hoisting Initial conditions Original Article Particle size Shock waves Thermodynamics Thickness Thin films Vertical orientation Wave dispersion Wave velocity |
title | Experimental research on dust lifting by propagating shock wave |
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