A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows

Mixtures of fluids and granular sediments play an important role in many industrial, geotechnical, and aerospace engineering problems, from waste management and transportation (liquid–sediment mixtures) to dust kick-up below helicopter rotors (gas–sediment mixtures). These mixed flows often involve...

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Main Authors: Baumgarten, Aaron S, Couchman, Benjamin LS, Kamrin, Ken
Other Authors: Massachusetts Institute of Technology. Department of Aeronautics and Astronautics
Format: Article
Language:English
Published: Elsevier BV 2022
Online Access:https://hdl.handle.net/1721.1/138830
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author Baumgarten, Aaron S
Couchman, Benjamin LS
Kamrin, Ken
author2 Massachusetts Institute of Technology. Department of Aeronautics and Astronautics
author_facet Massachusetts Institute of Technology. Department of Aeronautics and Astronautics
Baumgarten, Aaron S
Couchman, Benjamin LS
Kamrin, Ken
author_sort Baumgarten, Aaron S
collection MIT
description Mixtures of fluids and granular sediments play an important role in many industrial, geotechnical, and aerospace engineering problems, from waste management and transportation (liquid–sediment mixtures) to dust kick-up below helicopter rotors (gas–sediment mixtures). These mixed flows often involve bulk motion of hundreds of billions of individual sediment particles and can contain both highly turbulent regions and static, non-flowing regions. This breadth of phenomena necessitates the use of continuum simulation methods, such as the material point method (MPM), which can accurately capture these large deformations while also tracking the Lagrangian features of the flow (e.g. the granular surface, elastic stress, etc.). Recent works using two-phase MPM frameworks to simulate these mixtures have shown substantial promise; however, these approaches are hindered by the numerical limitations of MPM when simulating pure fluids. In addition to the well-known particle ringing instability and difficulty defining inflow/outflow boundary conditions, MPM has a tendency to accumulate quadrature errors as materials deform, increasing the rate of overall error growth as simulations progress. In this work, we present an improved, two-phase continuum simulation framework that uses the finite volume method (FVM) to solve the fluid phase equations of motion and MPM to solve the solid phase equations of motion, substantially reducing the effect of these errors and providing better accuracy and stability for long-duration simulations of these mixtures.
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spelling mit-1721.1/1388302024-06-07T20:16:12Z A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows Baumgarten, Aaron S Couchman, Benjamin LS Kamrin, Ken Massachusetts Institute of Technology. Department of Aeronautics and Astronautics Massachusetts Institute of Technology. Department of Mechanical Engineering Mixtures of fluids and granular sediments play an important role in many industrial, geotechnical, and aerospace engineering problems, from waste management and transportation (liquid–sediment mixtures) to dust kick-up below helicopter rotors (gas–sediment mixtures). These mixed flows often involve bulk motion of hundreds of billions of individual sediment particles and can contain both highly turbulent regions and static, non-flowing regions. This breadth of phenomena necessitates the use of continuum simulation methods, such as the material point method (MPM), which can accurately capture these large deformations while also tracking the Lagrangian features of the flow (e.g. the granular surface, elastic stress, etc.). Recent works using two-phase MPM frameworks to simulate these mixtures have shown substantial promise; however, these approaches are hindered by the numerical limitations of MPM when simulating pure fluids. In addition to the well-known particle ringing instability and difficulty defining inflow/outflow boundary conditions, MPM has a tendency to accumulate quadrature errors as materials deform, increasing the rate of overall error growth as simulations progress. In this work, we present an improved, two-phase continuum simulation framework that uses the finite volume method (FVM) to solve the fluid phase equations of motion and MPM to solve the solid phase equations of motion, substantially reducing the effect of these errors and providing better accuracy and stability for long-duration simulations of these mixtures. 2022-01-05T18:29:48Z 2022-01-05T18:29:48Z 2021-10-01 2021-05-14 2022-01-05T18:25:02Z Article http://purl.org/eprint/type/JournalArticle 0045-7825 https://hdl.handle.net/1721.1/138830 Aaron S. Baumgarten, Benjamin L.S. Couchman, Ken Kamrin, A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows, Computer Methods in Applied Mechanics and Engineering, Volume 384, 2021 en 10.1016/J.CMA.2021.113940 Computer Methods in Applied Mechanics and Engineering Creative Commons Attribution-NonCommercial-NoDerivs License http://creativecommons.org/licenses/by-nc-nd/4.0/ application/pdf Elsevier BV arXiv
spellingShingle Baumgarten, Aaron S
Couchman, Benjamin LS
Kamrin, Ken
A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows
title A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows
title_full A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows
title_fullStr A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows
title_full_unstemmed A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows
title_short A coupled finite volume and material point method for two-phase simulation of liquid–sediment and gas–sediment flows
title_sort coupled finite volume and material point method for two phase simulation of liquid sediment and gas sediment flows
url https://hdl.handle.net/1721.1/138830
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