The InSight HP$^3$ mole on Mars: Lessons learned from attempts to penetrate to depth in the Martian soil
T. Spohn (1,2), T.L. Hudson (3), L. Witte (4), T. Wippermann (4), L., Wisniewski (5), B. Kediziora (5), C. Vrettos (6), R. D. Lorenz (7), M., Golombek (3), R. Lichtenfeld (8), M. Grott (2), J. Knollenberg (2), C. Krause, (9), C. Fantinati (9), S. Nagihara (10)

TL;DR
The InSight HP3 mole on Mars faced challenges penetrating the soil due to unexpected resistance and recoil issues, leading to lessons on designing more robust systems for future planetary subsurface exploration.
Contribution
This paper provides a detailed analysis of the failure modes of the InSight HP3 mole and offers design lessons for future planetary penetrators.
Findings
Mole only penetrated 40 cm due to cohesive duricrust.
Recoil and insufficient hammer energy limited penetration depth.
Martian soil resistance exceeded expectations.
Abstract
The NASA InSight mission payload includes the Heat Flow and Physical Properties Package HP to measure the surface heat flow. The package was designed to use a small penetrator -- nicknamed the mole -- to implement a string of temperature sensors in the soil to a depth of 5m. The mole itself is equipped with sensors to measure a thermal conductivity as it proceeds to depth. The heat flow would be calculated from the product of the temperature gradient and the thermal conductivity. To avoid the perturbation caused by annual surface temperature variations, the measurements would be taken at a depth between 3 m and 5 m. The mole was designed to penetrate cohesionless soil similar to Quartz sand which was expected to provide a good analogue material for Martian sand. The sand would provide friction to the buried mole hull to balance the remaining recoil of the mole hammer mechanism that…
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