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...
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
EDP Sciences
2017-01-01
|
Series: | EPJ Web of Conferences |
Online Access: | https://doi.org/10.1051/epjconf/201714003056 |
id |
doaj-59f9ee2e1e244668b829205ba7e45920 |
---|---|
record_format |
Article |
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 AT sobralyd effectofgeometricbaseroughnessonsizesegregation |
_version_ |
1721240619547885568 |