Seasonal Variations of Soil Thermal Conductivity at the InSight Landing Site

Abstract The heat flow and physical properties package measured soil thermal conductivity at the landing site in the 0.03–0.37 m depth range. Six measurements spanning solar longitudes from 8.0° to 210.0° were made and atmospheric pressure at the site was simultaneously measured using InSight's...

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Main Authors: M. Grott, S. Piqueux, T. Spohn, J. Knollenberg, C. Krause, E. Marteau, T. L. Hudson, F. Forget, L. Lange, N. Müller, M. Golombek, S. Nagihara, P. Morgan, J. P. Murphy, M. Siegler, S. D. King, D. Banfield, S. E. Smrekar, W. B. Banerdt
Format: Article
Language:English
Published: Wiley 2023-04-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2023GL102975
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author M. Grott
S. Piqueux
T. Spohn
J. Knollenberg
C. Krause
E. Marteau
T. L. Hudson
F. Forget
L. Lange
N. Müller
M. Golombek
S. Nagihara
P. Morgan
J. P. Murphy
M. Siegler
S. D. King
D. Banfield
S. E. Smrekar
W. B. Banerdt
author_facet M. Grott
S. Piqueux
T. Spohn
J. Knollenberg
C. Krause
E. Marteau
T. L. Hudson
F. Forget
L. Lange
N. Müller
M. Golombek
S. Nagihara
P. Morgan
J. P. Murphy
M. Siegler
S. D. King
D. Banfield
S. E. Smrekar
W. B. Banerdt
author_sort M. Grott
collection DOAJ
description Abstract The heat flow and physical properties package measured soil thermal conductivity at the landing site in the 0.03–0.37 m depth range. Six measurements spanning solar longitudes from 8.0° to 210.0° were made and atmospheric pressure at the site was simultaneously measured using InSight's Pressure Sensor. We find that soil thermal conductivity strongly correlates with atmospheric pressure. This trend is compatible with predictions of the pressure dependence of thermal conductivity for unconsolidated soils under martian atmospheric conditions, indicating that heat transport through the pore filling gas is a major contributor to the total heat transport. Therefore, any cementation or induration of the soil sampled by the experiments must be minimal and soil surrounding the mole at depths below the duricrust is likely unconsolidated. Thermal conductivity data presented here are the first direct evidence that the atmosphere interacts with the top most meter of material on Mars.
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spelling doaj-art-8375f9df268b4825b7808b60df5fb60e2025-08-20T02:04:21ZengWileyGeophysical Research Letters0094-82761944-80072023-04-01507n/an/a10.1029/2023GL102975Seasonal Variations of Soil Thermal Conductivity at the InSight Landing SiteM. Grott0S. Piqueux1T. Spohn2J. Knollenberg3C. Krause4E. Marteau5T. L. Hudson6F. Forget7L. Lange8N. Müller9M. Golombek10S. Nagihara11P. Morgan12J. P. Murphy13M. Siegler14S. D. King15D. Banfield16S. E. Smrekar17W. B. Banerdt18German Aerospace Center (DLR) Institute of Planetary Research Berlin GermanyJet Propulsion Laboratory California Institute of Technology Pasadena CA USAGerman Aerospace Center (DLR) Institute of Planetary Research Berlin GermanyGerman Aerospace Center (DLR) Institute of Planetary Research Berlin GermanyGerman Aerospace Center (DLR) MUSC Space Operations and Astronaut Training Cologne GermanyJet Propulsion Laboratory California Institute of Technology Pasadena CA USAJet Propulsion Laboratory California Institute of Technology Pasadena CA USALaboratoire de Météorologie Dynamique (LMD/IPSL/CNRS) Sorbonne Université Paris FranceLaboratoire de Météorologie Dynamique (LMD/IPSL/CNRS) Sorbonne Université Paris FranceGerman Aerospace Center (DLR) Institute of Planetary Research Berlin GermanyJet Propulsion Laboratory California Institute of Technology Pasadena CA USADepartment of Geosciences Texas Tech University Lubbock TX USAColorado Geological Survey Colorado School of Mines Golden CO USAVirginia Polytechnic Institute and State University Blacksburg VA USAPlanetary Science Institute Tucson AZ USAVirginia Polytechnic Institute and State University Blacksburg VA USACornell University Ithaca NY USAJet Propulsion Laboratory California Institute of Technology Pasadena CA USAJet Propulsion Laboratory California Institute of Technology Pasadena CA USAAbstract The heat flow and physical properties package measured soil thermal conductivity at the landing site in the 0.03–0.37 m depth range. Six measurements spanning solar longitudes from 8.0° to 210.0° were made and atmospheric pressure at the site was simultaneously measured using InSight's Pressure Sensor. We find that soil thermal conductivity strongly correlates with atmospheric pressure. This trend is compatible with predictions of the pressure dependence of thermal conductivity for unconsolidated soils under martian atmospheric conditions, indicating that heat transport through the pore filling gas is a major contributor to the total heat transport. Therefore, any cementation or induration of the soil sampled by the experiments must be minimal and soil surrounding the mole at depths below the duricrust is likely unconsolidated. Thermal conductivity data presented here are the first direct evidence that the atmosphere interacts with the top most meter of material on Mars.https://doi.org/10.1029/2023GL102975InSightHP3thermal conductivitysoilheat transport
spellingShingle M. Grott
S. Piqueux
T. Spohn
J. Knollenberg
C. Krause
E. Marteau
T. L. Hudson
F. Forget
L. Lange
N. Müller
M. Golombek
S. Nagihara
P. Morgan
J. P. Murphy
M. Siegler
S. D. King
D. Banfield
S. E. Smrekar
W. B. Banerdt
Seasonal Variations of Soil Thermal Conductivity at the InSight Landing Site
Geophysical Research Letters
InSight
HP3
thermal conductivity
soil
heat transport
title Seasonal Variations of Soil Thermal Conductivity at the InSight Landing Site
title_full Seasonal Variations of Soil Thermal Conductivity at the InSight Landing Site
title_fullStr Seasonal Variations of Soil Thermal Conductivity at the InSight Landing Site
title_full_unstemmed Seasonal Variations of Soil Thermal Conductivity at the InSight Landing Site
title_short Seasonal Variations of Soil Thermal Conductivity at the InSight Landing Site
title_sort seasonal variations of soil thermal conductivity at the insight landing site
topic InSight
HP3
thermal conductivity
soil
heat transport
url https://doi.org/10.1029/2023GL102975
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