Lagrangian-based Simulations of Hypervelocity Impact Experiments on Mars Regolith Proxy

被引:10
|
作者
Froment, M. [1 ,2 ]
Rougier, E. [2 ]
Larmat, C. [2 ]
Lei, Z. [2 ]
Euser, B. [2 ]
Kedar, S. [3 ]
Richardson, J. E. [4 ]
Kawamura, T. [5 ]
Lognonne, P. [5 ]
机构
[1] Ecole Normale Super Paris Saclay, Cachan, France
[2] Los Alamos Natl Lab, Earth & Environm Div, Los Alamos, NM 87545 USA
[3] CALTECH, Jet Prop Lab, Pasadena, CA USA
[4] Planetary Sci Inst, Tucson, AZ USA
[5] Univ Paris, Inst Phys Globe Paris, CNRS, Paris, France
关键词
Parametric study; Lagrangian numerical model; Shock wave; granular media; Mars regolith; Impact; CRATERING RATE; BEHAVIOR; ELEMENT;
D O I
10.1029/2020GL087393
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Most of the surface of Mars is covered with unconsolidated rocky material, known as regolith. High-fidelity models of the dynamics of impacts in such material are needed to help with the interpretation of seismic signals that are now recorded by SEIS, the seismometer of InSight. We developed a numerical model for impacts on regolith, using the novel Hybrid Optimization Software Suite (HOSS), which is a Lagrangian code mixing finite and discrete element formulations. We use data from hypervelocity impact experiments performed on pumice sand at the NASA Ames Vertical Gun Range to identify and calibrate key model parameters. The model provides insight into the plastic-elastic transition observed in the data and it also demonstrates that gravity plays a key role in the material response. Waveforms for receivers situated vertically below the impact point are correctly modeled, while more research is needed to explain the shallow receivers' signals.
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页数:8
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