Effect of geometric base roughness on size segregation

The geometric roughness at boundaries has a profound impact on the dynamics of granular flows. For a bumpy base made of fixed particles, two major factors have been separately studied in the literature, namely, the size and spatial distribution of base particles. A recent work (Jing et al. 2016) has...

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Main Authors: Jing L., Kwok C. Y., Leung Y. F., Sobral Y. D.
Format: Article
Language:English
Published: EDP Sciences 2017-01-01
Series:EPJ Web of Conferences
Online Access:https://doi.org/10.1051/epjconf/201714003056
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spelling doaj-59f9ee2e1e244668b829205ba7e459202021-08-02T06:01:08ZengEDP SciencesEPJ Web of Conferences2100-014X2017-01-011400305610.1051/epjconf/201714003056epjconf162384Effect of geometric base roughness on size segregationJing L.0Kwok C. Y.1Leung Y. F.2Sobral Y. D.3Department of Civil Engineering, The University of Hong KongDepartment of Civil Engineering, The University of Hong KongDepartment of Civil and Environmental Engineering, The Hong Kong Polytechnic UniversityDepartamento de Matemática, Universidade de Brasília, Campus Universitário Darcy RibeiroThe geometric roughness at boundaries has a profound impact on the dynamics of granular flows. For a bumpy base made of fixed particles, two major factors have been separately studied in the literature, namely, the size and spatial distribution of base particles. A recent work (Jing et al. 2016) has proposed a roughness indicator Ra, which combines both factors for any arbitrary bumpy base comprising equally-sized spheres. It is shown in mono-disperse flows that as Ra increases, a transition occurs from slip (Ra < 0.51) to non-slip (Ra > 0.62) conditions. This work focuses on such a phase transition in bi-disperse flows, in which Ra can be a function of time. As size segregation takes place, large particles migrate away from the bottom, leading to a variation of size ratio between flow- and base-particles. As a result, base roughness Ra evolves with the progress of segregation. Consistent with the slip/non-slip transition in mono-disperse flows, basal sliding arises at low values of Ra and the development of segregation might be affected; when Ra increases to a certain level (Ra > 0.62), non-slip condition is respected. This work extends the validity of Ra to bi-disperse flows, which can be used to understand the geometric boundary effect during segregation.https://doi.org/10.1051/epjconf/201714003056
collection DOAJ
language English
format Article
sources DOAJ
author Jing L.
Kwok C. Y.
Leung Y. F.
Sobral Y. D.
spellingShingle Jing L.
Kwok C. Y.
Leung Y. F.
Sobral Y. D.
Effect of geometric base roughness on size segregation
EPJ Web of Conferences
author_facet Jing L.
Kwok C. Y.
Leung Y. F.
Sobral Y. D.
author_sort Jing L.
title Effect of geometric base roughness on size segregation
title_short Effect of geometric base roughness on size segregation
title_full Effect of geometric base roughness on size segregation
title_fullStr Effect of geometric base roughness on size segregation
title_full_unstemmed Effect of geometric base roughness on size segregation
title_sort effect of geometric base roughness on size segregation
publisher EDP Sciences
series EPJ Web of Conferences
issn 2100-014X
publishDate 2017-01-01
description The geometric roughness at boundaries has a profound impact on the dynamics of granular flows. For a bumpy base made of fixed particles, two major factors have been separately studied in the literature, namely, the size and spatial distribution of base particles. A recent work (Jing et al. 2016) has proposed a roughness indicator Ra, which combines both factors for any arbitrary bumpy base comprising equally-sized spheres. It is shown in mono-disperse flows that as Ra increases, a transition occurs from slip (Ra < 0.51) to non-slip (Ra > 0.62) conditions. This work focuses on such a phase transition in bi-disperse flows, in which Ra can be a function of time. As size segregation takes place, large particles migrate away from the bottom, leading to a variation of size ratio between flow- and base-particles. As a result, base roughness Ra evolves with the progress of segregation. Consistent with the slip/non-slip transition in mono-disperse flows, basal sliding arises at low values of Ra and the development of segregation might be affected; when Ra increases to a certain level (Ra > 0.62), non-slip condition is respected. This work extends the validity of Ra to bi-disperse flows, which can be used to understand the geometric boundary effect during segregation.
url https://doi.org/10.1051/epjconf/201714003056
work_keys_str_mv AT jingl effectofgeometricbaseroughnessonsizesegregation
AT kwokcy effectofgeometricbaseroughnessonsizesegregation
AT leungyf effectofgeometricbaseroughnessonsizesegregation
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