Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog

The first seismometer operating on the surface of another planet was deployed by the NASA InSight (Interior Exploration using Seismic Investigations, Geodesy and Heat Transport) mission to Mars. It gives us an opportunity to investigate the seismicity of Mars, including any seismic activity caused b...

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Main Authors: Rajšić, Andrea, Miljkovic, Katarina, Collins, G.S., Wünnemann, K., Daubar, I.J., Wójcicka, N., Wieczorek, M.A.
Format: Journal Article
Language:English
Published: AMER GEOPHYSICAL UNION 2021
Subjects:
Online Access:http://purl.org/au-research/grants/arc/DE180100584
http://hdl.handle.net/20.500.11937/90194
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author Rajšić, Andrea
Miljkovic, Katarina
Collins, G.S.
Wünnemann, K.
Daubar, I.J.
Wójcicka, N.
Wieczorek, M.A.
author_facet Rajšić, Andrea
Miljkovic, Katarina
Collins, G.S.
Wünnemann, K.
Daubar, I.J.
Wójcicka, N.
Wieczorek, M.A.
author_sort Rajšić, Andrea
building Curtin Institutional Repository
collection Online Access
description The first seismometer operating on the surface of another planet was deployed by the NASA InSight (Interior Exploration using Seismic Investigations, Geodesy and Heat Transport) mission to Mars. It gives us an opportunity to investigate the seismicity of Mars, including any seismic activity caused by small meteorite bombardment. Detectability of impact generated seismic signals is closely related to the seismic efficiency, defined as the fraction of the impactor's kinetic energy transferred into the seismic energy in a target medium. This work investigated the seismic efficiency of the Martian near surface associated with small meteorite impacts on Mars. We used the iSALE-2D (Impact-Simplified Arbitrary Lagrangian Eulerian) shock physics code to simulate the formation of the meter-size impact craters, and we used a recently formed 1.5 m diameter crater as a case study. The Martian crust was simulated as unfractured nonporous bedrock, fractured bedrock with 25% porosity, and highly porous regolith with 44% and 65% porosity. We used appropriate strength and porosity models defined in previous works, and we identified that the seismic efficiency is very sensitive to the speed of sound and elastic threshold in the target medium. We constrained the value of the impact-related seismic efficiency to be between the order of ∼10-7 to 10-6 for the regolith and ∼10-4 to 10-3 for the bedrock. For new impacts occurring on Mars, this work can help understand the near-surface properties of the Martian crust, and it contributes to the understanding of impact detectability via seismic signals as a function of the target media.
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spelling curtin-20.500.11937-901942023-02-20T07:51:37Z Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog Rajšić, Andrea Miljkovic, Katarina Collins, G.S. Wünnemann, K. Daubar, I.J. Wójcicka, N. Wieczorek, M.A. Science & Technology Physical Sciences Geochemistry & Geophysics impact cratering InSight mission iSALE&#8208 2D code Mars numerical modeling seismic efficiency METEORITE IMPACTS ELYSIUM PLANITIA MARS EXPLOSION The first seismometer operating on the surface of another planet was deployed by the NASA InSight (Interior Exploration using Seismic Investigations, Geodesy and Heat Transport) mission to Mars. It gives us an opportunity to investigate the seismicity of Mars, including any seismic activity caused by small meteorite bombardment. Detectability of impact generated seismic signals is closely related to the seismic efficiency, defined as the fraction of the impactor's kinetic energy transferred into the seismic energy in a target medium. This work investigated the seismic efficiency of the Martian near surface associated with small meteorite impacts on Mars. We used the iSALE-2D (Impact-Simplified Arbitrary Lagrangian Eulerian) shock physics code to simulate the formation of the meter-size impact craters, and we used a recently formed 1.5 m diameter crater as a case study. The Martian crust was simulated as unfractured nonporous bedrock, fractured bedrock with 25% porosity, and highly porous regolith with 44% and 65% porosity. We used appropriate strength and porosity models defined in previous works, and we identified that the seismic efficiency is very sensitive to the speed of sound and elastic threshold in the target medium. We constrained the value of the impact-related seismic efficiency to be between the order of ∼10-7 to 10-6 for the regolith and ∼10-4 to 10-3 for the bedrock. For new impacts occurring on Mars, this work can help understand the near-surface properties of the Martian crust, and it contributes to the understanding of impact detectability via seismic signals as a function of the target media. 2021 Journal Article http://hdl.handle.net/20.500.11937/90194 10.1029/2020JE006662 English http://purl.org/au-research/grants/arc/DE180100584 http://purl.org/au-research/grants/arc/DP180100661 http://creativecommons.org/licenses/by-nc/3.0/ AMER GEOPHYSICAL UNION fulltext
spellingShingle Science & Technology
Physical Sciences
Geochemistry & Geophysics
impact cratering
InSight mission
iSALE&#8208
2D code
Mars
numerical modeling
seismic efficiency
METEORITE IMPACTS
ELYSIUM PLANITIA
MARS
EXPLOSION
Rajšić, Andrea
Miljkovic, Katarina
Collins, G.S.
Wünnemann, K.
Daubar, I.J.
Wójcicka, N.
Wieczorek, M.A.
Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog
title Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog
title_full Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog
title_fullStr Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog
title_full_unstemmed Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog
title_short Seismic Efficiency for Simple Crater Formation in the Martian Top Crust Analog
title_sort seismic efficiency for simple crater formation in the martian top crust analog
topic Science & Technology
Physical Sciences
Geochemistry & Geophysics
impact cratering
InSight mission
iSALE&#8208
2D code
Mars
numerical modeling
seismic efficiency
METEORITE IMPACTS
ELYSIUM PLANITIA
MARS
EXPLOSION
url http://purl.org/au-research/grants/arc/DE180100584
http://purl.org/au-research/grants/arc/DE180100584
http://hdl.handle.net/20.500.11937/90194