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Numerical simulations of aggregate breakup in bounded and unbounded turbulent flows
Breakup of small aggregates in fully developed turbulence is studied by means of direct numerical simulations in a series of typical bounded and unbounded flow configurations, such as a turbulent channel flow, a developing boundary layer and homogeneous isotropic turbulence. The simplest criterion f...
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Published in: | Journal of fluid mechanics 2015-03, Vol.766, p.104-128 |
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creator | Babler, Matthaus U. Biferale, Luca Brandt, Luca Feudel, Ulrike Guseva, Ksenia Lanotte, Alessandra S. Marchioli, Cristian Picano, Francesco Sardina, Gaetano Soldati, Alfredo Toschi, Federico |
description | Breakup of small aggregates in fully developed turbulence is studied by means of direct numerical simulations in a series of typical bounded and unbounded flow configurations, such as a turbulent channel flow, a developing boundary layer and homogeneous isotropic turbulence. The simplest criterion for breakup is adopted, whereby aggregate breakup occurs when the local hydrodynamic stress
${\it\sigma}\sim {\it\varepsilon}^{1/2}$
, with
${\it\varepsilon}$
being the energy dissipation at the position of the aggregate, overcomes a given threshold
${\it\sigma}_{cr}$
, which is characteristic for a given type of aggregate. Results show that the breakup rate decreases with increasing threshold. For small thresholds, it develops a scaling behaviour among the different flows. For high thresholds, the breakup rates show strong differences between the different flow configurations, highlighting the importance of non-universal mean-flow properties. To further assess the effects of flow inhomogeneity and turbulent fluctuations, the results are compared with those obtained in a smooth stochastic flow. Furthermore, we discuss the limitations and applicability of a set of independent proxies. |
doi_str_mv | 10.1017/jfm.2015.13 |
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${\it\sigma}\sim {\it\varepsilon}^{1/2}$
, with
${\it\varepsilon}$
being the energy dissipation at the position of the aggregate, overcomes a given threshold
${\it\sigma}_{cr}$
, which is characteristic for a given type of aggregate. Results show that the breakup rate decreases with increasing threshold. For small thresholds, it develops a scaling behaviour among the different flows. For high thresholds, the breakup rates show strong differences between the different flow configurations, highlighting the importance of non-universal mean-flow properties. To further assess the effects of flow inhomogeneity and turbulent fluctuations, the results are compared with those obtained in a smooth stochastic flow. Furthermore, we discuss the limitations and applicability of a set of independent proxies.</description><identifier>ISSN: 0022-1120</identifier><identifier>ISSN: 1469-7645</identifier><identifier>EISSN: 1469-7645</identifier><identifier>DOI: 10.1017/jfm.2015.13</identifier><language>eng</language><publisher>Cambridge, UK: Cambridge University Press</publisher><subject>Aggregates ; Boundary layers ; Breakup ; breakup/coalescence ; Channel flow ; Computational fluid dynamics ; Computer simulation ; Configurations ; Energy dissipation ; Energy exchange ; Fluids ; Hydrodynamics ; Inhomogeneity ; Isotropic turbulence ; multiphase and particle-laden flows ; Physics ; Scaling ; Studies ; Thresholds ; Turbulence ; Turbulent flow ; turbulent flows ; Variation</subject><ispartof>Journal of fluid mechanics, 2015-03, Vol.766, p.104-128</ispartof><rights>2015 Cambridge University Press</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c337t-993717349b0e2badf2c102da23d14770c10f716392d1e6e011f1902b395f0a303</citedby><cites>FETCH-LOGICAL-c337t-993717349b0e2badf2c102da23d14770c10f716392d1e6e011f1902b395f0a303</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0022112015000130/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>230,314,776,780,881,27901,27902,72703</link.rule.ids><backlink>$$Uhttps://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-161602$$DView record from Swedish Publication Index$$Hfree_for_read</backlink></links><search><creatorcontrib>Babler, Matthaus U.</creatorcontrib><creatorcontrib>Biferale, Luca</creatorcontrib><creatorcontrib>Brandt, Luca</creatorcontrib><creatorcontrib>Feudel, Ulrike</creatorcontrib><creatorcontrib>Guseva, Ksenia</creatorcontrib><creatorcontrib>Lanotte, Alessandra S.</creatorcontrib><creatorcontrib>Marchioli, Cristian</creatorcontrib><creatorcontrib>Picano, Francesco</creatorcontrib><creatorcontrib>Sardina, Gaetano</creatorcontrib><creatorcontrib>Soldati, Alfredo</creatorcontrib><creatorcontrib>Toschi, Federico</creatorcontrib><title>Numerical simulations of aggregate breakup in bounded and unbounded turbulent flows</title><title>Journal of fluid mechanics</title><addtitle>J. Fluid Mech</addtitle><description>Breakup of small aggregates in fully developed turbulence is studied by means of direct numerical simulations in a series of typical bounded and unbounded flow configurations, such as a turbulent channel flow, a developing boundary layer and homogeneous isotropic turbulence. The simplest criterion for breakup is adopted, whereby aggregate breakup occurs when the local hydrodynamic stress
${\it\sigma}\sim {\it\varepsilon}^{1/2}$
, with
${\it\varepsilon}$
being the energy dissipation at the position of the aggregate, overcomes a given threshold
${\it\sigma}_{cr}$
, which is characteristic for a given type of aggregate. Results show that the breakup rate decreases with increasing threshold. For small thresholds, it develops a scaling behaviour among the different flows. For high thresholds, the breakup rates show strong differences between the different flow configurations, highlighting the importance of non-universal mean-flow properties. To further assess the effects of flow inhomogeneity and turbulent fluctuations, the results are compared with those obtained in a smooth stochastic flow. Furthermore, we discuss the limitations and applicability of a set of independent proxies.</description><subject>Aggregates</subject><subject>Boundary layers</subject><subject>Breakup</subject><subject>breakup/coalescence</subject><subject>Channel flow</subject><subject>Computational fluid dynamics</subject><subject>Computer simulation</subject><subject>Configurations</subject><subject>Energy dissipation</subject><subject>Energy exchange</subject><subject>Fluids</subject><subject>Hydrodynamics</subject><subject>Inhomogeneity</subject><subject>Isotropic turbulence</subject><subject>multiphase and particle-laden flows</subject><subject>Physics</subject><subject>Scaling</subject><subject>Studies</subject><subject>Thresholds</subject><subject>Turbulence</subject><subject>Turbulent flow</subject><subject>turbulent flows</subject><subject>Variation</subject><issn>0022-1120</issn><issn>1469-7645</issn><issn>1469-7645</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNptkF1LwzAYhYMoOKdX_oGAl9L5vknXmMsxP2HohR-3IW2T2q1tZtIw_Pd2zK8Lrw4HHh4Oh5BThAkCioulbScMcDpBvkdGmGYyEVk63ScjAMYSRAaH5CiEJQBykGJEnh5ia3xd6IaGuo2N7mvXBeos1VXlTaV7Q3Nv9Cquad3R3MWuNCXVXUlj99366PPYmK6ntnGbcEwOrG6COfnKMXm5uX6e3yWLx9v7-WyRFJyLPpGSCxQ8lTkYluvSsgKBlZrxElMhYGhWYMYlK9FkBhAtSmA5l1MLmgMfk2TnDRuzjrla-7rV_kM5Xaur-nWmnK_Uqn9TmGEGbODPdvzau_doQq-WLvpumKhQSja9TEXKB-p8RxXeheCN_fEiqO3LanhZbV9WyH83FLrNfV1W5o_0H_4TWQB-Xg</recordid><startdate>20150310</startdate><enddate>20150310</enddate><creator>Babler, Matthaus U.</creator><creator>Biferale, Luca</creator><creator>Brandt, Luca</creator><creator>Feudel, Ulrike</creator><creator>Guseva, Ksenia</creator><creator>Lanotte, Alessandra S.</creator><creator>Marchioli, Cristian</creator><creator>Picano, 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simulations of aggregate breakup in bounded and unbounded turbulent flows</title><author>Babler, Matthaus U. ; Biferale, Luca ; Brandt, Luca ; Feudel, Ulrike ; Guseva, Ksenia ; Lanotte, Alessandra S. ; Marchioli, Cristian ; Picano, Francesco ; Sardina, Gaetano ; Soldati, Alfredo ; Toschi, Federico</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c337t-993717349b0e2badf2c102da23d14770c10f716392d1e6e011f1902b395f0a303</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Aggregates</topic><topic>Boundary layers</topic><topic>Breakup</topic><topic>breakup/coalescence</topic><topic>Channel flow</topic><topic>Computational fluid dynamics</topic><topic>Computer simulation</topic><topic>Configurations</topic><topic>Energy dissipation</topic><topic>Energy exchange</topic><topic>Fluids</topic><topic>Hydrodynamics</topic><topic>Inhomogeneity</topic><topic>Isotropic 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Fluid Mech</addtitle><date>2015-03-10</date><risdate>2015</risdate><volume>766</volume><spage>104</spage><epage>128</epage><pages>104-128</pages><issn>0022-1120</issn><issn>1469-7645</issn><eissn>1469-7645</eissn><abstract>Breakup of small aggregates in fully developed turbulence is studied by means of direct numerical simulations in a series of typical bounded and unbounded flow configurations, such as a turbulent channel flow, a developing boundary layer and homogeneous isotropic turbulence. The simplest criterion for breakup is adopted, whereby aggregate breakup occurs when the local hydrodynamic stress
${\it\sigma}\sim {\it\varepsilon}^{1/2}$
, with
${\it\varepsilon}$
being the energy dissipation at the position of the aggregate, overcomes a given threshold
${\it\sigma}_{cr}$
, which is characteristic for a given type of aggregate. Results show that the breakup rate decreases with increasing threshold. For small thresholds, it develops a scaling behaviour among the different flows. For high thresholds, the breakup rates show strong differences between the different flow configurations, highlighting the importance of non-universal mean-flow properties. To further assess the effects of flow inhomogeneity and turbulent fluctuations, the results are compared with those obtained in a smooth stochastic flow. Furthermore, we discuss the limitations and applicability of a set of independent proxies.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.1017/jfm.2015.13</doi><tpages>25</tpages></addata></record> |
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subjects | Aggregates Boundary layers Breakup breakup/coalescence Channel flow Computational fluid dynamics Computer simulation Configurations Energy dissipation Energy exchange Fluids Hydrodynamics Inhomogeneity Isotropic turbulence multiphase and particle-laden flows Physics Scaling Studies Thresholds Turbulence Turbulent flow turbulent flows Variation |
title | Numerical simulations of aggregate breakup in bounded and unbounded turbulent flows |
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