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A Numerical Model of the SEIS Leveling System Transfer Matrix and Resonances: Application to SEIS Rotational Seismology and Dynamic Ground Interaction
Authors:Lucile Fayon  Brigitte Knapmeyer-Endrun  Philippe Lognonné  Marco Bierwirth  Aron Kramer  Pierre Delage  Foivos Karakostas  Sharon Kedar  Naomi Murdoch  Raphael F Garcia  Nicolas Verdier  Sylvain Tillier  William T Pike  Ken Hurst  Cédric Schmelzbach  William B Banerdt
Institution:1.Institut de Physique du Globe de Paris-Sorbonne Paris Cité,Université Paris Diderot,Paris,France;2.Earthquake Observatory Bensberg,University of Cologne,Bergish Gladbach,Germany;3.Max Planck Institute for Solar System Research,G?ttingen,Germany;4.Laboratoire Navier (CERMES),Ecole des Ponts ParisTech,Paris,France;5.Jet Propulsion Laboratory (JPL),California Institut of Technology,Pasadena,USA;6.Institut Supérieur de l’Aéronautique et de l’Espace (ISAE-SUPAERO),Université de Toulouse,Toulouse,France;7.Centre National d’Etudes Spatiales (CNES),Toulouse,France;8.Imperial College,London,United Kingdom;9.ETH,Zurich,Switzerland
Abstract:Both sensors of the SEIS instrument (VBBs and SPs) are mounted on the mechanical leveling system (LVL), which has to ensure a level placement on the Martian ground under currently unknown local conditions, and provide the mechanical coupling of the seismometers to the ground. We developed a simplified analytical model of the LVL structure in order to reproduce its mechanical behavior by predicting its resonances and transfer function. This model is implemented numerically and allows to estimate the effects of the LVL on the data recorded by the VBBs and SPs on Mars. The model is validated through comparison with the horizontal resonances (between 35 and 50 Hz) observed in laboratory measurements. These modes prove to be highly dependent of the ground horizontal stiffness and torque. For this reason, an inversion study is performed and the results are compared with some experimental measurements of the LVL feet’s penetration in a martian regolith analog. This comparison shows that the analytical model can be used to estimate the elastic ground properties of the InSight landing site. Another application consists in modeling the 6 sensors on the LVL at their real positions, also considering their sensitivity axes, to study the performances of the global SEIS instrument in translation and rotation. It is found that the high frequency ground rotation can be measured by SEIS and, when compared to the ground acceleration, can provide ways to estimate the phase velocity of the seismic surface waves at shallow depths. Finally, synthetic data from the active seismic experiment made during the HP3 penetration and SEIS rotation noise are compared and used for an inversion of the Rayleigh phase velocity. This confirms the perspectives for rotational seismology with SEIS which will be developed with the SEIS data acquired during the commissioning phase after landing.
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