TY - GEN
T1 - Data-driven Characterization of Crater Morphology During Plume-surface Interaction
AU - Bruni, Lorenzo
AU - Patel, Meet
AU - Evrard, Fabien
AU - Capecelatro, Jesse
AU - Villafañe, Laura
N1 - This work was supported by the Early Stage Innovations Grant No. 80NSSC24K0276 from the National Aeronautics and Space Administration.
PY - 2025
Y1 - 2025
N2 - The impingement of high-speed rocket plumes on regolith surfaces during propulsive landings on the surface of the Moon or planetary bodies erodes a crater and lifts ejecta that can compromise the lander and nearby infrastructure. There is a lack of engineering models that can aid risk prediction, stemming from an incomplete understanding of plume-surface interactions (PSI) and the diverse erosion mechanisms dominating in different regimes. In this work, we use data from recent sub-scale PSI experiments performed at NASA to advance the current understanding of erosion phenomenology and cratering predictions. Experiments involved a supersonic jet impinging on a granular bed, with a splitter plate aligned with the jet axis allowing visual access to the crater cross-section. This work uses the high-speed imagery of the crater as it evolves under the action of the jet. Custom image-analysis methodologies are used to extract the profile of the crater as the granular surface is eroded. For some of the test cases, the crater shape can be approximated using a family of standard Gaussian curves, which enables crater profiles to be defined with minimal parameters. Using the symbolic regression framework PySINDy, a dynamical system is identified that reduces the crater evolution to a set of ordinary differential equations. The dynamical system generated and presented in this work showed a good agreement with the experimental data.
AB - The impingement of high-speed rocket plumes on regolith surfaces during propulsive landings on the surface of the Moon or planetary bodies erodes a crater and lifts ejecta that can compromise the lander and nearby infrastructure. There is a lack of engineering models that can aid risk prediction, stemming from an incomplete understanding of plume-surface interactions (PSI) and the diverse erosion mechanisms dominating in different regimes. In this work, we use data from recent sub-scale PSI experiments performed at NASA to advance the current understanding of erosion phenomenology and cratering predictions. Experiments involved a supersonic jet impinging on a granular bed, with a splitter plate aligned with the jet axis allowing visual access to the crater cross-section. This work uses the high-speed imagery of the crater as it evolves under the action of the jet. Custom image-analysis methodologies are used to extract the profile of the crater as the granular surface is eroded. For some of the test cases, the crater shape can be approximated using a family of standard Gaussian curves, which enables crater profiles to be defined with minimal parameters. Using the symbolic regression framework PySINDy, a dynamical system is identified that reduces the crater evolution to a set of ordinary differential equations. The dynamical system generated and presented in this work showed a good agreement with the experimental data.
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U2 - 10.2514/6.2025-2568
DO - 10.2514/6.2025-2568
M3 - Conference contribution
AN - SCOPUS:105001414978
SN - 9781624107238
T3 - AIAA Science and Technology Forum and Exposition, AIAA SciTech Forum 2025
BT - AIAA Science and Technology Forum and Exposition, AIAA SciTech Forum 2025
PB - American Institute of Aeronautics and Astronautics Inc, AIAA
T2 - AIAA Science and Technology Forum and Exposition, AIAA SciTech Forum 2025
Y2 - 6 January 2025 through 10 January 2025
ER -