Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheology
A key mechanism by which geophysical flows evolve is mass exchange with the underlying bed, either by entraining material from the bed, or by depositing material. Although it is known that some consequences of these mass exchange processes include changes in the volume, momentum and local rheology o...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
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EDP Sciences
2023-01-01
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| Series: | E3S Web of Conferences |
| Online Access: | https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/52/e3sconf_dfhm82023_01008.pdf |
| _version_ | 1797740258146648064 |
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| author | Goodwin Saoirse Robin Piton Guillaume Chambon Guillaume |
| author_facet | Goodwin Saoirse Robin Piton Guillaume Chambon Guillaume |
| author_sort | Goodwin Saoirse Robin |
| collection | DOAJ |
| description | A key mechanism by which geophysical flows evolve is mass exchange with the underlying bed, either by entraining material from the bed, or by depositing material. Although it is known that some consequences of these mass exchange processes include changes in the volume, momentum and local rheology of the flow, the circumstances under which specific changes occur are not well-established. Given the enormous number of competing mechanisms present in geophysical flows, it is not surprising that the state of the art for modelling entrainment is essentially still empirical. In this study, we implement a Herschel-Bulkley (non-Newtonian) rheology into an existing open-source Smoothed Particle Hydrodynamics solver (DualSPHysics). This rheology can reasonably represent clay-rich flows, typical of those observed in the French Prealps. We hence undertake a highly-idealised, quantitative investigation of entrainment mechanisms for flows overriding non-fixed beds. For the beds, we vary the yield stress and the depth. Preliminary results reveal a rich variety of behaviours that can be obtained for different bed properties, including both acceleration and deceleration of the flow material. These mechanisms are reminiscent (but not identical) of observations from other studies where geo-materials were used. |
| first_indexed | 2024-03-12T14:09:52Z |
| format | Article |
| id | doaj.art-9bf3115f022b45358dd23a294c79847d |
| institution | Directory Open Access Journal |
| issn | 2267-1242 |
| language | English |
| last_indexed | 2024-03-12T14:09:52Z |
| publishDate | 2023-01-01 |
| publisher | EDP Sciences |
| record_format | Article |
| series | E3S Web of Conferences |
| spelling | doaj.art-9bf3115f022b45358dd23a294c79847d2023-08-21T09:02:29ZengEDP SciencesE3S Web of Conferences2267-12422023-01-014150100810.1051/e3sconf/202341501008e3sconf_dfhm82023_01008Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheologyGoodwin Saoirse Robin0Piton Guillaume1Chambon Guillaume2Univ. Grenoble-Alpes, INRAE, UR ETNAUniv. Grenoble-Alpes, INRAE, UR ETNAUniv. Grenoble-Alpes, INRAE, UR ETNAA key mechanism by which geophysical flows evolve is mass exchange with the underlying bed, either by entraining material from the bed, or by depositing material. Although it is known that some consequences of these mass exchange processes include changes in the volume, momentum and local rheology of the flow, the circumstances under which specific changes occur are not well-established. Given the enormous number of competing mechanisms present in geophysical flows, it is not surprising that the state of the art for modelling entrainment is essentially still empirical. In this study, we implement a Herschel-Bulkley (non-Newtonian) rheology into an existing open-source Smoothed Particle Hydrodynamics solver (DualSPHysics). This rheology can reasonably represent clay-rich flows, typical of those observed in the French Prealps. We hence undertake a highly-idealised, quantitative investigation of entrainment mechanisms for flows overriding non-fixed beds. For the beds, we vary the yield stress and the depth. Preliminary results reveal a rich variety of behaviours that can be obtained for different bed properties, including both acceleration and deceleration of the flow material. These mechanisms are reminiscent (but not identical) of observations from other studies where geo-materials were used.https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/52/e3sconf_dfhm82023_01008.pdf |
| spellingShingle | Goodwin Saoirse Robin Piton Guillaume Chambon Guillaume Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheology E3S Web of Conferences |
| title | Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheology |
| title_full | Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheology |
| title_fullStr | Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheology |
| title_full_unstemmed | Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheology |
| title_short | Mass exchange between geophysical flows and beds: Idealised computational modelling using a Herschel-Bulkley rheology |
| title_sort | mass exchange between geophysical flows and beds idealised computational modelling using a herschel bulkley rheology |
| url | https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/52/e3sconf_dfhm82023_01008.pdf |
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