The local distribution of stress near a point of zero shear stress in a rectilinear flow field
The distribution of stress in the vicinity of a point at which shear stress magnitude is zero is investigated analytically for rectilinear flow of a fluid in a channel or pipe. For a fluid with non-linear power-law properties the contours of constant stress and velocity either approach circular or f...
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Language: | English |
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Cambridge University Press (CUP)
1974
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Online Access: | http://dx.doi.org/10.1017/s0022143000023455 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023455 |
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crcambridgeupr:10.1017/s0022143000023455 2024-03-03T08:46:02+00:00 The local distribution of stress near a point of zero shear stress in a rectilinear flow field Raymond, Charles F. 1974 http://dx.doi.org/10.1017/s0022143000023455 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023455 en eng Cambridge University Press (CUP) Journal of Glaciology volume 13, issue 67, page 141-143 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1974 crcambridgeupr https://doi.org/10.1017/s0022143000023455 2024-02-08T08:37:11Z The distribution of stress in the vicinity of a point at which shear stress magnitude is zero is investigated analytically for rectilinear flow of a fluid in a channel or pipe. For a fluid with non-linear power-law properties the contours of constant stress and velocity either approach circular or flat shapes near such a point, irrespective of the particular boundary conditions. There are no intermediate cases, although such intermediate behavior exists for linear fluids. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 13 67 141 143 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Raymond, Charles F. The local distribution of stress near a point of zero shear stress in a rectilinear flow field |
topic_facet |
Earth-Surface Processes |
description |
The distribution of stress in the vicinity of a point at which shear stress magnitude is zero is investigated analytically for rectilinear flow of a fluid in a channel or pipe. For a fluid with non-linear power-law properties the contours of constant stress and velocity either approach circular or flat shapes near such a point, irrespective of the particular boundary conditions. There are no intermediate cases, although such intermediate behavior exists for linear fluids. |
format |
Article in Journal/Newspaper |
author |
Raymond, Charles F. |
author_facet |
Raymond, Charles F. |
author_sort |
Raymond, Charles F. |
title |
The local distribution of stress near a point of zero shear stress in a rectilinear flow field |
title_short |
The local distribution of stress near a point of zero shear stress in a rectilinear flow field |
title_full |
The local distribution of stress near a point of zero shear stress in a rectilinear flow field |
title_fullStr |
The local distribution of stress near a point of zero shear stress in a rectilinear flow field |
title_full_unstemmed |
The local distribution of stress near a point of zero shear stress in a rectilinear flow field |
title_sort |
local distribution of stress near a point of zero shear stress in a rectilinear flow field |
publisher |
Cambridge University Press (CUP) |
publishDate |
1974 |
url |
http://dx.doi.org/10.1017/s0022143000023455 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023455 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 13, issue 67, page 141-143 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000023455 |
container_title |
Journal of Glaciology |
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13 |
container_issue |
67 |
container_start_page |
141 |
op_container_end_page |
143 |
_version_ |
1792501859717480448 |