Resumen
The broadcloth material used in parachute manufacturing is generally a thin, woven, permeable textile. The relatively small length scales of the pores and gaps inside the fabric make it challenging to resolve these features in a full-scale parachute simulation. Simulations are performed using a 3D reconstruction of the geometry of the material used in the Mars 2020 mission, and simulation results using the detailed reconstructed geometry are compared to the simplified model previously proposed in (Huang, D. Z., Wong, M. L., Lele, S. K., and Farhat, C., “Homogenized Flux-Body Force Treatment of Compressible Viscous Porous Wall Boundary Conditions,” AIAA Journal, Vol. 59, No. 6, 2021, pp. 2045–2059). Furthermore, results from simulations under Earth ambient lab conditions are compared to experimental permeability test data to verify the choice of a simplified geometry required for some reduced-order models. A series of simulations under ASPIRE SR03 flight conditions are also performed to study the permeability of the fabric in a rarefied flow regime. The flow inside the material is shown to be similar to a developing pipe flow that does not reach a fully developed state. Significant slip velocity is observed inside the individual pores in the material, and the pressure drag is found to be the primary contributor to the overall material drag. The previous analytical pipe flow solution based on a simplified pore geometry solution predicts a higher total drag by only a small amount (∼ 0.8%) compared to the results presented in this work. Therefore, while flow through the parachute material at the micro-scale shows interesting physics, adding more complex assumptions to simplified models, such as a slip wall boundary condition and rarefied effects, likely increases the computational cost and complexity without significantly changing the predicted drag on the material.
| Idioma original | English |
|---|---|
| Título de la publicación alojada | AIAA Aviation Forum and ASCEND, 2024 |
| Estado | Published - 2024 |
| Evento | AIAA Aviation Forum and ASCEND, 2024 - Las Vegas, United States Duración: jul 29 2024 → ago 2 2024 |
Serie de la publicación
| Nombre | AIAA Aviation Forum and ASCEND, 2024 |
|---|
Conference
| Conference | AIAA Aviation Forum and ASCEND, 2024 |
|---|---|
| País/Territorio | United States |
| Ciudad | Las Vegas |
| Período | 7/29/24 → 8/2/24 |
Nota bibliográfica
Publisher Copyright:© 2024, American Institute of Aeronautics and Astronautics Inc, AIAA. All rights reserved.
Financiación
Parts of this work were performed at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not constitute or imply its endorsement by the United States Government or the Jet Propulsion Laboratory, California Institute of Technology. Simulations in this work used the Anvil cluster at Purdue University through allocation MCH230049 from the Advanced Cyberinfrastructure Coordination Ecosystem: Services & Support (ACCESS) program, which is supported by National Science Foundation grants #2138259, #2138286, #2138307, #2137603, and #2138296. S.Danial Ghasimi acknowledges partial support from the Jet Propulsion Laboratory, California Institute of Technology, through Subcontract No. 1691016.
| Financiadores | Número del financiador |
|---|---|
| National Aeronautics and Space Administration | |
| Jet Propulsion Laboratory | |
| National Science Foundation Arctic Social Science Program | 2138286, 2138296, 2137603, 2138307, 2138259 |
| California Institute of Technology | 1691016 |
| Purdue Climate Change Research Center, Purdue University | MCH230049 |
ASJC Scopus subject areas
- Energy Engineering and Power Technology
- Nuclear Energy and Engineering
- Aerospace Engineering
- Space and Planetary Science
Huella
Profundice en los temas de investigación de 'Permeability Modeling of Mars Parachute Broadcloth Materials'. En conjunto forman una huella única.Citar esto
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