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Beagle 2 PAW and ARM

Beagle 2 lander at the Airbus Stevenage facility before integration with Mars Express, lid open. The base section is about 0.7 m in diameter and holds the instruments; the solar panels are stowed in the lid. The stowed ARM and the PAW occupy the upper right of the base Source: Bridges et al. 2017, Royal Society Open Science, figure 4 [2]; CC BY 4.0.

Beagle 2 carried a five-degree-of-freedom manipulator, the Anthropomorphic Robotic Manipulator, terminating in a fixed instrument cluster called the Position Adjustable Workbench [1]. The PAW is not an end effector in the usual sense: it is the payload, carrying the stereo cameras, microscope, X-ray spectrometer, Mossbauer spectrometer, rock corer grinder, wind sensor, wide angle mirror, torch, spoon and the launch tube for the PLUTO subsurface mole. The arm exists to point that cluster.

The lander landed on Mars on 25 December 2003 and was never heard from [2]. It was identified in HiRISE imagery in 2014 and 2015 and the identification published in 2017; the configuration seen is consistent with lid deployment and partial solar panel deployment, which would have left the UHF antenna covered [2].

The design driver is mass. Landed mass was 33.18 kg against a 69 kg probe mass limit, of which the scientific payload was 8.896 kg, and the program aimed at the highest ratio of payload to support systems flown to Mars, achievable only with an integrated design and minimal or zero redundancy [1]. The complete experiment package draws less than 40 W.

ParameterValue
ARM degrees of freedom5, with the PAW permanently attached at the wrist
ARM length, fully extended109 cm, body joint center to PAW wrist joint center
Joint actuatorDC brushed motor through a 100:1 harmonic gearbox
Joint position sensingpotentiometer on the output shaft
Typical joint speed0.6 deg/s, axes 1 to 3
Forearm plus PAW length400 mm
Contact sensingpiezoelectric force load washer, 3 pC/N
Stop delay after contact detectionabout 100 ms
ARM mass2.11 kg
PAW mass2.75 kg
Rock corer grinder mass348 g flight model, without translation table
Rock corer grinder envelopeabout 30 by 60 by 100 mm
Rock corer grinder power6 W
Grinding depthup to 6 mm of weathering rind
Ground patch diameter10 mm
PLUTO total mass890 g: 340 g mole, 550 g deployment unit
PLUTO envelopeabout 380 by 90 by 80 mm, mole 280 mm long
PLUTO power3 W, 17 W for the post-landing pin-puller release
Mole sampling depth, vertical1.5 m baselined
Mole temperature measurement depth1.25 m maximum
Mole sample volumeabout 0.20 cm3
Mole hammer intervalone shock every 5 s
Mole lateral travel per strokeabout 10 mm
Spoon sample volumeno more than 20 mm3
Onboard processorERC32
Comms bands and ratesUHF, forward 2 and 8 kbit/s, return 2 to 128 kbit/s
Battery42-cell lithium ion
Solar arrayfour deployable panels, about 1 m2 effective, triple-junction GaAs on germanium

Values from [1].

ParameterValueSource
Landing siteIsidis Planitia, 265.0 W, 11.6 N[1]
Landing date25 December 2003[2]
Planned primary missionup to 180 sols[1]
Planned complete sampling cycles5 to 6 samples over about 80 to 100 sols
Rocks planned for full in situ analysisabout 3
Mole samples planned in the primary missionabout 3
Relay assetsMars Express and Mars Odyssey
Outcomelanded, no contact; identified in HiRISE imagery[2]

Each ARM joint is a DC brushed motor driving a 100:1 harmonic gearbox, with a potentiometer mounted directly on the output shaft for position [1]. Typical joint speed is 0.6 deg/s on axes 1 to 3. The arm is not a general-purpose manipulator: with the PAW fixed to the wrist, every instrument placement is an arm placement, and the requirements levied on the ARM are optical rather than mechanical. Digital elevation model construction of the 0.6 to 1.2 m near-stereo working zone requires the PAW to view the scene from at least two or three perspectives while holding targets in focus; the 360 degree multispectral panorama requires the PAW to point straight up for height advantage and rotate about that axis; the close-up lens works at about 80 mm standoff, which constrains PAW orientation to avoid surface contamination and navigational hazards [1]. Contact is detected by a piezoelectric force load washer of 3 pC/N sensitivity, which produces charge when the PAW meets a resistive surface: a rock, a calibration target, the gas analysis package inlet or a sample dish. The sensor is quiet during normal gentle arm motion, so it functions as a contact event detector rather than a force sensor. After contact is detected the arm continues to drive for a short interval set by joint stiffness, stopping about 100 ms after detection, with the exact time depending on the instrument being placed and the expected PAW orientation relative to the surface [1]. Approach forces for each instrument are then derived from that point as a function of arm velocity, direction and time, and the weight of the PAW or its vertical component can be used at a suitably chosen site. Final approach precision comes from single-joint motion. Moving the elbow alone, with a forearm and PAW length of 400 mm, the PAW sweeps forward up to 5 mm in the worst case to prepare a surface with the rock corer grinder, which corresponds to about 0.7 degrees of tool sweep, within the surface preparation accuracy the grinder achieves [1]. The X-ray spectrometer was proposed for all first contacts with a candidate sample because it tolerates contact loads better than the other instruments, establishing a reference point from which subsequent positioning is more accurate.

The arm operates with a degree of autonomy because communication windows are limited, but it is not intelligent: it executes predetermined maneuvers and strategies [1]. A set of configurations designated safe points is defined within the sphere of PAW and ARM operations, and advancement toward a target proceeds until contact is detected or a timeout expires, in which case corrective action may abort the sequence and return the arm to a safe or default position.

The PAW carries the in situ instruments and the tools that prepare samples for them and deliver material to the gas analysis package on the lander deck [1]. That package is a 6 cm radius magnetic sector mass spectrometer that runs in both static and dynamic modes, and it is the instrument that every PAW tool and the mole feed. Institutional responsibility was distributed: the X-ray spectrometer and the wide angle mirror, torch and spoon to the University of Leicester, the stereo camera system to Mullard Space Science Laboratory, the microscope to Bern, PLUTO and the sampling mole to DLR Cologne, the rock corer grinder to Hong Kong Polytechnic University and the wind sensor to Oxford, with Leicester supplying the PAW structure, control electronics and cabling.

ElementFunction
Stereo camera systempanoramic and working-zone stereo imaging through filters, close-up lens at about 80 mm
Microscopeself-illuminating, contact required, images individual grains, 4 micrometer per pixel scale
X-ray spectrometerelemental composition, Mg to Nb, Fe-55 and Cm-244 style excitation after Viking rather than the APXS proton mode
Mossbauer spectrometeriron-bearing mineralogy of the prepared surface
Rock corer grinderremoves weathering rind and cores the ground patch for delivery to the gas analysis package
PLUTO molesubsurface soil sampling, subsurface temperature, soil mechanics from intrusion behavior
Spoonbackup sampling of unconsolidated soil
Wide angle mirror360 degree first view of the site through the right stereo camera before the PAW is unstowed
Wind sensorboundary layer wind regime at the PAW

Elements and functions from [1].

The wide angle mirror is a deployment safety device as much as an instrument: it is held under spring tension until the lid and solar panels open, then moves into the field of view of the right-hand stereo camera, giving a panorama that lets mission planners unstow the PAW without hitting anything [1]. The rock corer grinder is dual function. Grinding removes up to 6 mm of weathering rind to produce individual or arrayed flat 10 mm diameter fresh surfaces sized for the spectrometers, and after in situ analysis the same tool cores the ground patch by a combined hammering and rotating action of the main drive, retaining chippings in a micro end effector jaw device and delivering a reproducible volume suited to the gas analysis package ovens [1]. A translation table developed for the qualification model would have swept the tool head to produce a flat area of about 30 mm diameter, but it was not adopted for flight on mass and other grounds [1].

PLUTO is a self-penetrating mole tethered to a support mechanism on the PAW, derived from a Russian self-burying penetrometer and scaled down for space under an ESA technology program [1]. Once a small initial penetration is achieved it needs no reaction force from the lander: an internal inertial hammering mechanism drives it forward, powered through the tether, and it can reach depths several times the length of its casing. At one shock every 5 s, reaching 1 m vertically was estimated at 30 minutes to 1 hour under Mars gravity and the expected soil resistance [1].

A commandable mechanism at the tip opens at the sampling depth to take about 0.20 cm3 of soil and closes to secure it [1]. Retrieval reverses the cable reel, pulling the mole back into the launch tube on the PAW while the arm holds position, after which the arm moves to the gas analysis package inlet port and the tip mechanism opens again to discharge. Retraction was tested on a variety of analog materials, and can be assisted by running the hammer while rewinding the cable, an option reserved for deep sampling.

Horizontal deployment uses the same hammering to crawl the mole across the surface at about 10 mm per percussive stroke, a mode verified in an earlier ESA technology activity [1]. The intended use was to reach a boulder beyond the reach of the PAW and then divert downward to sample the protected soil beneath its overhang. Beyond sampling, the mole was to act as a platform for subsurface temperature measurement against time and depth, and its intrusion behavior was to yield soil mechanical properties and layering. The rationale for a 1.5 m mole is stated directly [1]: Viking reached only 20 cm, which remained inside a presumably highly oxidized layer in which no organic matter was measured, and the top meter of bulk soil is expected to have been exposed to atmosphere and ultraviolet flux by aeolian mixing, destroying organics on a decadal scale. There is no precise positioning requirement for the mole, unlike the instruments.

Lander electronics carry an ERC32 processor and provide power conditioning, distribution and management plus the instrument and equipment interfaces [1]. Onboard software is in four modules: a bootstrap loader in PROM that runs mission phase detection and executes the application image; common software providing low-level drivers and utilities; probe software covering entry, descent and landing and handover; and lander software providing subsystem control and experiment functionality. The last three are stored in EEPROM and loaded into RAM for execution.

Power comes from a 42-cell lithium ion battery kept warm overnight by insulation and heater power, charged by four deployable panels of about 1 m2 total effective area using triple-junction gallium arsenide cells on germanium substrates [1]. Communication is UHF only, bidirectional with Mars Express and Mars Odyssey, at 2 and 8 kbit/s forward and 2 to 128 kbit/s return, with receive and transmit antennas integrated into the lander lid structure.

The post-landing sequence is fully automatic: deploy solar panels, start battery charging for the remainder of the day, take a monochrome image with the right stereo camera and the wide angle mirror positioned automatically in the field of view, and enter an overnight low-power mode if no contact occurs on sol 1, continuing in low power with daytime charging until communication is possible [1].

Once contact is established and the first image assessed, the PAW and ARM are deployed to a safe default configuration and an imaging phase builds the stereo coverage needed for a digital elevation model of the working zone [1]. Thereafter the sol is split by power budget rather than by science priority: arm positioning and gas analysis package processes run during the day, and low-resource activities such as spectrometry and microscopy run at night. A complete sampling cycle was estimated at tens of sols, and the primary mission was sized at 80 to 100 sols of sampling with a target lifetime of up to 180 sols [1].

No signal was received after landing. High Resolution Imaging Science Experiment coverage of the 57 by 7.6 km landing ellipse led to a candidate identification in 2014, and further targeted imaging with super-resolution processing supported it [2]. The identification rests on an object about 1.5 m across with a distinctive multilobed shape, high reflectivity against the local terrain, specular reflections, and a position close to the center of the planned ellipse. HiRISE has 25 cm per pixel resolution, so the lander is a few pixels across and its configuration is partly masked by those specular reflections [2]. What can be resolved is consistent with deployment of the lid and then some or all of the solar panels. Each panel is 0.57 m in diameter and the fully deployed lander is 1.7 m across, with the panels at 20 degrees to the horizontal when fully deployed [2].

Failure to deploy all four panels is a sufficient explanation for the silence, because the UHF antenna is exposed only when the last panel opens [2]. Entry, descent and landing therefore appear to have worked, with only the final panel deployment failing. Everything downstream of that, including the ARM, the PAW and PLUTO, was never exercised on Mars.

PLUTO is the program’s transferable product: a self-penetrating tethered mole requiring no reaction force from the lander after initial penetration, capable of both vertical burial and horizontal crawling on the same hammer mechanism, and carrying its own temperature sensing and soil-mechanics inference [1]. The PAW itself is an architectural argument that did not recur: rather than an arm carrying interchangeable tools to instruments mounted on the body, Beagle 2 fixed the entire in situ instrument suite to the wrist, which removes every sample transfer step between instruments at the cost of making arm placement accuracy the limiting factor for all of them. The contact strategy that follows, a piezoelectric charge detector used as an event trigger with a fixed post-contact drive interval set by joint stiffness, is the minimum-mass alternative to a force-torque sensor. The mass discipline is the other legacy: 8.896 kg of payload and less than 40 W on a 33.18 kg landed vehicle, accepted with minimal or zero redundancy [1].

References

  1. Pullan, D., Sims, M. R., Wright, I. P., Pillinger, C. T. and Trautner, R. (2004). Beagle 2: the Exobiological Lander of Mars Express. ESA Publications Division. Source
    BibTeX
    @incollection{pullan2004beagle,
      title = {Beagle 2: the Exobiological Lander of Mars Express},
      author = {Pullan, Derek and Sims, Mark R. and Wright, Ian P. and Pillinger, Colin T. and Trautner, Roland},
      booktitle = {Mars Express: The Scientific Payload, ESA SP-1240},
      pages = {165--204},
      year = {2004},
      publisher = {ESA Publications Division},
      url = {https://sci.esa.int/documents/33745/35957/1567255011803-BeagleWeb.pdf}
    }
  2. Bridges, J. C., Clemmet, J., Croon, M., Sims, M. R., Pullan, D., Muller, H. G. M., Tao, Y., Xiong, S.-T., Putri, A. R., Parker, T., Turner, S. M. R. and Pillinger, J. M. (2017). Identification of the Beagle 2 lander on Mars. Royal Society Open Science, 10. Source
    BibTeX
    @article{bridges2017identification,
      title = {Identification of the Beagle 2 lander on Mars},
      author = {Bridges, John C. and Clemmet, Jim and Croon, Mark and Sims, Mark R. and Pullan, Derek and Muller, Howell G. M. and Tao, Yu and Xiong, Si-Ting and Putri, Alfiah R. and Parker, Tim and Turner, Simon M. R. and Pillinger, Jeremy M.},
      journal = {Royal Society Open Science},
      volume = {4},
      number = {10},
      pages = {170785},
      year = {2017},
      doi = {10.1098/rsos.170785},
      url = {https://europepmc.org/articles/PMC5666264}
    }

Further reading

  • Griffiths, A. D., Coates, A. J., Josset, J.-L., Paar, G., Hofmann, B., Pullan, D., Rüffer, P., Sims, M. R. and Pillinger, C. T. (2005). The Beagle 2 Stereo Camera System. Planetary and Space Science. Source
  • (2026). ESA: Beagle 2 lander. sci.esa.int/web/mars-express/-/31157-beagle-2-lander
  • NASA. (2020). Cross-Program Design Specification for Natural Environments (DSNE), Revision G. NASA Marshall Space Flight Center. Source
  • Justh, H. L., Burns, K. L., Dutta, S. and Hoffman, J. (2024). Mars Global Reference Atmospheric Model (Mars-GRAM) 2024: User Guide. NASA Marshall Space Flight Center. Source