InSight mission

In­Sight – a geo­phys­i­cal ob­ser­va­to­ry for Mars

Artist’s impression of the NASA InSight lander on the Martian surface
Artist’s im­pres­sion of the NASA In­Sight lan­der on the Mar­tian sur­face
Credit: NASA/JPL-Caltech.

Artist’s impression of the NASA InSight lander on the Martian surface

Launched on 5 May 2018, NASA’s In­Sight space­craft will land on 26 Novem­ber, just north of the Mar­tian equa­tor, and de­ploy its so­lar pan­els. SEIS, an in­stru­ment for record­ing seis­mic waves (left of im­age), and HP3, an in­stru­ment de­vel­oped by DLR to mea­sure the ther­mal con­duc­tiv­i­ty of the Mar­tian re­golith and the heat flow from the in­te­ri­or of the plan­et (right of im­age), will be placed on the sur­face of the plan­et pos­si­bly be­fore the turn of the year.

The NASA Insight mission was launched on 5 May 2018. In this mission, a lander will carry out geophysical measurements directly on the surface of Mars to explore the planet’s inner structure and thermal balance. The German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR) has contributed to this mission in the form of the Heat Flow and Physical Properties Package HP3. On 26 November 2018, InSight landed north of the equator, on the Elysium Planitia plain. Following a test phase, the experiments will commence after the 2018/19 turn of the year. The duration of the mission is initially set at one Mars year, which corresponds to approximately two Earth years.

The expense of space travel and the mass and energy that would be required rule out the creation of specialised observatories on Mars for cost reasons, so the alternative option of creating an observatory as a payload, equipped with several instruments has been chosen for the InSight mission. The idea of installing networks of several stations at the same time was also deemed too risky and expensive. As such, InSight will be the first and, for the time being, the only geophysical observatory to fly to Mars. Scientists have developed new technology for the mission in order to get as much scientific value out of the station as possible.

InSight was proposed in 2011 as an entry to the NASA Discovery competition, and selected in August 2012. The scientists were able to draw upon a large number of earlier suggestions, particularly from Europe. The European Space Agency (ESA) looked more closely at two MarsNet and InterMarsnet proposals, while the French space agency CNES examined the most recent NetLander proposals from 2000–2003. NASA had also carried out preliminary studies in the form of the Mars Environmental SURvey (MESUR) and the Gravity and Extreme Magnetism Small Explorer (GEMS). One feature of the mission is that it combines US expertise in lander technology with European competence in geophysical instruments.

First measurements of heat flow from the interior of the planet and marsquakes

While InSight is a Mars-based mission, scientists are interested in investigating rocky planets in general. Of these, they have a relatively detailed knowledge of Earth. InSight is now intended to allow a reasonably accurate determination of the interior structure and an insight into the formation of an Earth-like planet. Mars is a good choice, as it is accessible as Earth’s planetary neighbour, while the surface conditions are manageable for terrestrial technology, unlike Venus, whose atmosphere is too hot at 400 degrees Celsius, not to mention highly corrosive. In addition, scientists believe Mars to be sufficiently representative of Earth-like planets, although such planets may have starkly different individual features.

Despite the financial constraints of this relatively small-scale Discovery mission, the key instruments required by a geophysical observatory are all present. These include the Seismic Experiment for Interior Structure (SEIS) and a heat flow probe – the Heat Flow and Physical Properties Probe (HP3). Weather sensors (atmospheric pressure and temperature) and a magnetometer are also on board as auxiliary instruments for the seismometer. With the help of the communications hardware, it will be possible to measure fluctuations in the orientation of the rotational axis using the Doppler effect. These fluctuations are caused by uneven distributions of mass within the planet. Such measurements can therefore help to determine Mars’ inner structure, one of the main aims of the mission.

Germany, the German Aerospace Centre (Deutsches Zentrum für Luft- und Raumfahrt; DLR) and its scientific institutes, in particular the DLR Institute of Planetary Research, are involved in the mission, as is the Max Planck Institute for Solar System Research in Göttingen.

Mars 'mole' HP3

DLR has provided the HP3 heat flow probe, which was developed by a team led by the Principal Investigator, Tilman Spohn from the DLR Institute of Planetary Research. Significant contributions to HP3 have also been made by the DLR institutes of Space Systems in Bremen, Optical Sensor Systems in Berlin, Space Operations and Astronaut Training at the facility in Cologne, System Dynamics and Control in Oberpfaffenhofen, Composite Structures and Adaptive Systems in Braunschweig, and Robotics and Mechatronics in Oberpfaffenhofen.

The Max Planck Institute for Solar System Research developed the mechanical system for levelling the seismometer and was financed by the DLR Space Administration in its capacity as Germany’s Space Agency.

  • Prof.Dr. Tilman Spohn
    HP³ Prin­ci­pal In­ves­ti­ga­tor
    Ger­man Aerospace Cen­ter (DLR)

    DLR In­sti­tute of Plan­e­tary Re­search
    Telephone: +49 30 67055-300
    Fax: +49 30 67055-303
    Linder Höhe
    51147 Köln
  • Elke Heinemann
    Ger­man Aerospace Cen­ter (DLR)
    Pub­lic Af­fairs and Com­mu­ni­ca­tions
    Telephone: +49 2203 601-2867
    Fax: +49 2203 601-3249

  • Ulrich Köhler
    Pub­lic re­la­tions co­or­di­na­tor
    Ger­man Aerospace Cen­ter (DLR)
    In­sti­tute of Plan­e­tary Re­search
    Telephone: +49 30 67055-215
    Fax: +49 30 67055-402
    Rutherfordstraße 2
    12489 Berlin
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