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  • The InSight Mission – Seismology on Mars and Beyond [Poster]
  • Characterization of the InSight Landing Site Near Surface Properties Using the Heat Flow and Physical Properties Probe (Hp3) Mole as a Seismic Source

 

Characterization of the InSight Landing Site Near Surface Properties Using the Heat Flow and Physical Properties Probe (Hp3) Mole as a Seismic Source

Date: 4/25/2019

Time: 06:00 PM

Room: Fifth Avenue

The InSight mission is the first Mars lander to place an ultra-sensitive broadband seismometer on the planet’s surface. About 1m away from the seismometer, a Heat Flow and Physical Properties Probe (HP3) experiment will hammer a probe down to 5m into the Martian subsurface to measure the heat coming from Mars' interior and reveal the planet's thermal history. The probe, which uses a self-hammering mechanism, will generate thousands of seismic signals that can be used to study the shallow subsurface.

The mission’s science objectives focus on planetary-scale seismic and tectonic processes and their implications to rocky planet formation. Nevertheless the proximity of a repeating hammer source to a sensitive seismometer presents a unique opportunity to carry out the first geotechnical study of the shallow Martian subsurface.

The HP3 mole hammering mechanism produces a distinct seismic signals, but using these signals for a geotechnical seismic profiling presents several challenges: (1) The InSight Seismic Experiment requires 100 samples-per-second data that results in under-sampling the HP3 signal; (2) Although each HP3 penetration session produces several hundred hammer strokes, the ~4s interval between them varies slightly with regolith properties and with mole temperature; (3) A second stroke, ~0.06s following the initial stroke, also varies in time, and may obscure a reflection from an anticipated basalt layer several meters below the surface.

In 2018, we conducted a field experiment to test the efficiency of data processing algorithms developed by the team. A site whose geological setting were intended to mimic the anticipated landing site was selected. A seismic survey of the shallow subsurface was conducted and a model of the underlying shallow geology was constructed. Subsequently, a simulation of the HP3-SEIS experiment was carried out, whose data was used to asses our ability to recover the seismic velocity in the vicinity of the InSight lander and the thickness of the regolith layer. We will report details of the analysis conducted by the team.

 


Presenting Author: Sharon Kedar


Authors

Sharon Kedar

Presenting Author Corresponding Author

sharon.kedar@jpl.nasa.gov

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, United States

Presenting Author
Corresponding Author

William B Banerdt

william.b.banerdt@jpl.nasa.gov

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, United States

Nienke Brinkman

nienke.brinkman@erdw.ethz.ch

ETH Zurich, Zurich, , Switzerland

Pierre Delage

pierre.delage@enpc.fr

École Nationale des Ponts et Chaussées, Paris, , France

Lucile Fayon

fayon@ipgp.fr

Institut de Physique du Globe de Paris, Paris, , France

Matthias Grott

matthias.grott@dlr.de

Deutsches Zentrum für Luft und Raumfahrt, Berlin, , Germany

Anna C Horleston

anna.horleston@bristol.ac.uk

University of Bristol, Bristol, , United Kingdom

Troy L Hudson

troy.l.hudson@jpl.nasa.gov

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, United States

Kenneth Hurst

kenneth.j.hurst@jpl.nasa.gov

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, United States

Aaron B Kiely

aaron.b.kiely@jpl.nasa.gov

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, United States

Brigitte Knapmeyer-Endrun

brigitte.knapmeyer-endrun@uni-koeln.de

University of Cologne, Cologne, , Germany

Christian Krause

christian.krause@dlr.de

Deutsches Zentrum für Luft und Raumfahrt, Berlin, , Germany

Philippe Lognonné

lognonne@ipgp.fr

Institut de Physique du Globe de Paris, Paris, , France

William T Pike

w.t.pike@imperial.ac.uk

Imperial College London, London, , United Kingdom

Johan O A Robertsson

johan.robertsson@erdw.ethz.ch

ETH Zurich, Zurich, , Switzerland

Cedric Schmelzbach

cedric.schmelzbach@erdw.ethz.ch

ETH Zurich, Zurich, , Switzerland

Nicholas C Schmerr

nschmerr@umd.edu

University of Maryland, College Park, Maryland, United States

Tilman C Spohn

tilman.spohn@dlr.de

Deutsches Zentrum für Luft und Raumfahrt, Berlin, , Germany

David Sollberger

david.sollberger@erdw.ethz.ch

ETH Zurich, Zurich, , Switzerland

Simon Stähler

simon.staehler@erdw.ethz.ch

ETH Zurich, Zurich, , Switzerland

Nicholas A Teanby

n.teanby@bristol.ac.uk

University of Bristol, Bristol, , United Kingdom

Martin van Driel

vandriel@erdw.ethz.ch

ETH Zurich, Zurich, , Switzerland

Christos Vrettos

vrettos@rhrk.uni-kl.de

Technical University Kaiserslautern, Kaiserslautern, , Germany

Characterization of the InSight Landing Site Near Surface Properties Using the Heat Flow and Physical Properties Probe (Hp3) Mole as a Seismic Source

Category

The InSight Mission – Seismology on Mars and Beyond

Description