Viking Surface Sampler
Program pages NASA Science: Viking 1
Source: brewbooks, via Wikimedia Commons [13]; CC BY-SA 2.0.
Overview
Section titled “Overview”A stationary lander on Mars cannot drive to a sample, and a lightbulb-length radio delay rules out driving a manipulator from Earth in real time. Whatever reached the surface material had to be commanded once, execute a whole acquisition and delivery cycle on its own, and survive doing so with no operator watching until the telemetry came back. The Viking Surface Sampler Subsystem was the first machine built to meet that problem and, in doing so, became the first machine to acquire and process extraterrestrial samples for onboard analysis on another planet [8], [1], [13]. Built by Martin Marietta Aerospace under NASA LaRC, one flew on each of Viking Lander 1 and Viking Lander 2, landing in 1976 [8], [9].
The subsystem is not a manipulator alone. It comprises the acquisition assembly, a furlable articulated boom carrying a collector head; the biology processing and distribution assembly; the gas chromatograph mass spectrometer processing and distribution assembly; and the electronics control assembly [10]. It interfaces with the biology instrument, the GCMS and the X-ray fluorescence spectrometer, and it also carries the hardware for the physical properties and magnetic properties investigations: mirrors on the side of the acquisition assembly, magnet arrays on the collector head backhoe, a magnet cleaning brush and a magnet magnification mirror.
Specifications
Section titled “Specifications”| Parameter | Value | Source |
|---|---|---|
| Boom type | furlable tube boom, flattened on the drum, forms a column when extended | [12] |
| Boom stowed length on drum | about 12 ft (3.7 m) wound on a 6 in (152 mm) drum | |
| Boom extension | 10 ft (3.0 m) | [9] |
| Acquisition assembly envelope | about 14 in high by 8.5 in wide by 24 in long (0.36 by 0.22 by 0.61 m) | [12] |
| Acquisition assembly mass | about 28 lb (12.7 kg) | |
| Primary sample field | 120 degree arc, 3 ft minimum to 10 ft maximum radius, about 90 sq ft (8.4 m2) | |
| Collector head | clamshell, motor-rotated lower jaw housing, solenoid-actuated upper jaw | [12] |
| Head rotation | 180 degrees, motor driven | |
| Jaw vibration | solenoid driven by an 8.8 Hz square wave | |
| Collector head sieve | 2000 micrometer holes in the lid, with disaggregation teeth inside | |
| Scooping force | collector head extended forward with 30 lbf (133 N) | |
| Backhoe furrow | about 3 in wide by 1 ft long (76 mm by 0.3 m) | |
| Backhoe instrumentation | two samarium-cobalt magnet arrays plus a magnifying mirror | |
| Jaw instrumentation | temperature probe on the lower jaw surface | |
| Boom position sensing | potentiometers inside the boom, 9-bit commanded position word | |
| Command interface | 16-bit digital commands from the lander guidance, control and sequencing computer |
Mission profile
Section titled “Mission profile”| Parameter | Value | Source |
|---|---|---|
| Landers carrying the subsystem | 2 | [9] |
| Planned deliveries, 90 sol mission | 4 to the biology PDA, 3 to the GCMS PDA | [12] |
| Viking Lander 1 first deliveries | sol 8, to biology, GCMS and XRFS | [9] |
| Boom anomalies, Viking Lander 1 | 2 | |
| Boom anomalies, Viking Lander 2 | 1 |
Acquisition assembly
Section titled “Acquisition assembly”About 12 ft of furlable boom is wound on a single 6 in diameter drum [12]. The element is forced flat as it is wound and forms a structural column when driven out through guides [12]. On the flight vehicle the boom extends 10 ft from the lander [9]. The collector head at the tip was designed to dig or scoop. The rotation motor sits in a cylindrical section immediately behind the jaw; the lower jaw housing is the largest single piece and the primary structure; the upper jaw is opened, closed and vibrated by a solenoid attached to the housing directly behind it.
The vibration mechanism is dual purpose and self-diagnosing. The solenoid is driven by an 8.8 Hz square wave [12], and a switch adjacent to the jaw monitors jaw movement and chops the drive signal, which produces a short sharp vibration suited to moving material. If the jaw hangs open because of excess load or material sticking, the switch does not chop and the full square wave is applied, giving much more violent jaw motion [12]. The backhoe on the reverse face was designed to acquire subsurface material and can also cut trenches, which were used to study wind effects on soil and angles of repose. It carries two samarium-cobalt magnet arrays viewable directly from behind by the lander cameras, and a magnifying mirror giving a close view of the front of the arrays. A temperature probe on the lower jaw surface records jaw temperature, and a grid pattern painted on the lander top deck provides a reference against which deposited material can be assessed for color, size, angle of repose and wind action.
Deployment and acquisition sequence
Section titled “Deployment and acquisition sequence”Deployment is a fixed opening sequence. Pyrotechnics release the covers on both processing and distribution assemblies and the wind spoilers deploy automatically. The furlable boom is then extended about 1.5 in to release the boom mechanism from its support post, the mechanism elevates about 45 degrees and rotates about 180 degrees in azimuth, the collector head rotates 45 degrees inside its protective shroud, and the boom extends approximately a further 4 in, which mechanically releases the shroud so that four springs propel it about eight feet clear through the thin atmosphere [12].
A surface acquisition then runs as a strictly serial sequence: azimuth rotation to a predetermined position, elevation to approximately horizontal, extension to about nine feet. Each motion is performed singly rather than simultaneously, which the designers adopted to improve system accuracy and increase safety [12]. The boom then elevates down until the ground contact switch in the collector head gimbal actuates, the jaw opens, and the head is driven forward with 30 lbf, filling the scoop. For a subsurface sample the boom retracts a short distance on ground contact [12], the backhoe is positioned and cuts a furrow about 3 in wide and a foot long, and the head then opens and moves forward to take material from the bottom of the furrow. The reachable field on the flight landers was about 130 sq ft in front of and between legs 2 and 3 [9]. Delivery inverts the head so that material lodged in recesses falls out, then rotates in azimuth over the target processing assembly, extends to center over its screen, and lowers to a height that allows half an inch of head vibration while remaining shielded from the wind by the spoilers atop the processor. The head is then vibrated [12]: the lid is pulsed in short strokes at 8.8 Hz, sharp teeth inside the cover break up loosely bound clods, and the 2000 micrometer holes sift material onto the primary screen. A level sensor in the metering tube reports whether enough material has arrived; if not, the head vibrates again and the level sensor rechecks after time is allowed for grinding and sieving.
Sample processing
Section titled “Sample processing”The GCMS processing and distribution assembly is a grinder and metering chain. An agitator, a spring wire shaped like a question mark, rubs the underside of the 2000 micrometer primary screen while its stem runs down the funnel into the grinder, where a lobe on the grinder agitates it, keeping material flowing and preventing compaction in the funnel [10]. Material passes into a comminutor that acts as an auger and grinder combined; free to position itself within its housing, its eccentric action grinds while the flutes reject material, in the manner of a drill forcing chips away from the cutting face, so material circulates until it is fine enough to fall through the 600 micrometer gap around the periphery of the auger. It then falls into a plenum chamber and is stirred over a 300 micrometer sieve covering a 1 cm3 metering tube [10]. When the level sensor reports the tube full, the tube is translated in a sliding shuttle to transfer material to the GCMS, then to a dump position where the shuttle vibrator runs and the comminutor is reversed; a linear cam lowers the auger to open the gap to 4000 micrometers so the flutes force oversized material through the dump tube into a self-contained dump box.
The biology assembly is functionally similar but has no grinder. It uses material directly as sifted through a 1000 micrometer primary screen, processes 7 cm3, is unpressurized, and breathes through a bio-filter in its upper cover, with its own integral dump box [10].
Organic cleanliness drove the manufacturing process. The biology assembly was cleaned to 1 ppm total organics at the Martin Marietta plant; the GCMS assembly and the collector head and shroud assemblies were cleaned at the NASA White Sands Test Facility to less than 1 nanogram per square centimeter using procedures developed for Apollo [10]. Assemblies were broken down as far as possible, each part cleaned, flushed, reassembled and vacuum baked. The parts finished so clean that a screw would not thread into an insert, so new screws with silver plating as lubricant were used for reassembly, and motors were hermetically sealed to retain their lubricants. Assemblies were then pressurized to exclude contaminants and stayed pressurized through testing, transport and spacecraft integration, relying on their own sealed construction to hold cleanliness until landing. Organic cleanliness of the sample path was a mission-level requirement because the GCMS was the instrument searching for organic material [9].
Control and avionics
Section titled “Control and avionics”The Surface Sampler Control Assembly sits inside the lander body and receives 16-bit digital commands from the lander guidance, control and sequencing computer, decoding each and activating the appropriate motor or solenoid [10]. For boom movements the command word carries 9 bits of position information. Potentiometers inside the boom return analog position to the control assembly, which digitizes and compares commanded against actual position, removing power from the boom when they agree. Each command is timed to assure completion before the next is issued. Because of the Earth-Mars transmission delay, every sampler operation is executed by onboard sequences and logic rather than by real-time control. The first sequence was stored in the lander computer before launch and could be wholly replaced by ground update. The software is organized as tables of detailed digital commands for specific operations, with decision elements tied to the level detectors and the flexibility to deliver a sample to any investigation or combination of them.
Qualification
Section titled “Qualification”Component-level qualification, subsystem-level tests and integration into a lander System Test Bed were completed before flight. Beyond the normal dynamic and thermal environments, sampler hardware was flown on the NASA and USAF KC-135 to reproduce the effects of reduced Martian gravity on the mechanism [10]. Development also ran late enough that the surface sampler boom motor appeared on the Viking project’s list of top problems tracked by program management [9].
Flight performance and anomalies
Section titled “Flight performance and anomalies”The Viking Lander 1 sampler produced three separate operational problems, all resolved by resequencing rather than by hardware workaround [9].
On sol 2 a boom no-go occurred because the boom was not commanded to extend far enough and a locking pin, part of the shroud latching system, did not drop free [9]. The pin was intended to fall to the Martian surface during boom extension, and the commanded extension in the stored sequence was too short to release it [12]. The failure was reproduced on the science test lander at JPL, and analysts calculated that extending the boom to about 35 cm would let the pin fall. Boom retraction was also constrained in the recovery plan, because at a certain point the boom extraction motor deliberately clutches and shuts itself off to avoid motor damage. New commands were issued on sol 5, the boom extended far enough, the pin fell free, and samples were delivered on sol 8 to the biology instrument, the GCMS and the XRFS.
The GCMS then did not indicate a full sample and its analysis was automatically deferred by the lander computer. A second acquisition was ordered, and another boom no-go occurred before delivery. Analysis established that this one was caused by commanding two successive retract sequences [9]. The GCMS analysis was started on the material already delivered and returned a successful result; the boom was subsequently exercised in extension and continued without further problems.
Viking Lander 2 flew with sequence changes derived from these events and did not repeat them, but had one of its own: on sol 8, after delivery to the biology experiment and before delivery to the XRFS, a boom no-go occurred [9]. Analysis and further testing concluded that a switch sensing collector head rotation had malfunctioned. Subsequent boom sequences were modified to remove the need for that signal, and no further sampler anomalies occurred; all remaining deliveries were made as scheduled.
Results returned
Section titled “Results returned”No Viking lander experiment was designed to measure physical properties, so the mechanical properties of the surface materials were inferred from lander data: touchdown dynamics, engine-exhaust erosion, sample trenches, surface-bearing tests, backhoe touchdowns and motor currents in the comminutor [11]. Three soil-like materials were distinguished. Drift material is fine grained with local planes of weakness, and is consistent with an angle of internal friction of about 18 degrees, cohesion of 0.7 to 3.0 kPa and a bulk density of 1200 kg/m³ [11]. Blocky material is consistent with about 30 degrees, cohesions of 1.5 to 16 kPa and 1600 kg/m³. Crusty to cloddy material is variable: about 35 degrees and 0.5 to 5.2 kPa where chiefly crusty to cloddy, about 31 degrees and 0.2 to 2.3 kPa where fines and crusts are mixed, with 1400 kg/m³ plausible for the Lander 2 site [11]. The 18 degree figure for drift material was itself treated as a puzzle in the report, since the trench estimates average 18.2 ± 2.6 degrees and few materials other than smooth glass spheres are that low; the authors raise the possibility that it is an apparent angle produced by pore gas pressure rather than a true one. Landing provided an independent measurement [11]: both landers touched down at about 2 m/s, and on Lander 1 footpad 2 penetrated drift material 0.165 m while footpad 3 penetrated blocky material 0.036 m. The environment those numbers describe, and the design allowances against it, are the ones later Mars surface missions were built to [2].
Technologies developed and later heritage
Section titled “Technologies developed and later heritage”The furlable flattened boom is the mechanism the program is remembered for: a 3 m reach and a 12 m2 workspace obtained from a boom stowed on a drum 152 mm in diameter [12], [9]. The collector head established the pattern later Mars samplers followed, a scoop with a secondary cutting element on the reverse face for harder material, a vibratory sieve integrated into the tool rather than placed downstream, and instrumentation carried on the tool itself for a separate investigation. The self-diagnosing vibrator, where a jaw-motion switch chops the drive waveform and a hung jaw automatically receives a more violent full-wave drive, is a mechanically implemented fault response with no software involvement. The organic cleanliness chain [12], cleaning to 1 ng/cm2 at White Sands, silver-plated fasteners as the only permitted lubricant on reassembly, hermetically sealed motors and pressurized storage through to landing, is the earliest flown implementation of an organically controlled sample path on another planet. The operational lesson was that a subsystem executing stored sequences with no real-time control needs its recovery paths in the sequence design: all four flight anomalies across the two landers were cured by changing commands, twice by extending a motion further than originally planned and once by ceasing to depend on a failed switch [12].
Every Mars surface sampler flown since has kept the two-jointed idea of a scoop for loose material and a harder-material tool riding beside or behind it, even where the mechanism inside changed completely. The Phoenix Robotic Arm replaced the furlable boom with a four-degree-of-freedom rigid arm and traded the backhoe for a rasp built into the back of the scoop, so a single tool could both dig icy soil and grind a harder ice-cemented layer before scooping the cuttings, and it used its own trenching and scraping motions as a soil mechanics instrument in the way the Viking backhoe had done [4], [5]. Mars Science Laboratory went further still, mounting a rotary-percussive drill and a hard-material scoop on the same turret so that either tool could be selected and then processed through an onboard sieving and portioning chain, CHIMRA, that plays the same role the Viking comminutor and metering tube played, reducing acquired material to a metered portion before delivery to an instrument [6], [7]. The Icebreaker drill concept, aimed at depths no flown Mars sampler has reached, still traces its own sample-acquisition history back to the Viking scoops as the first excavators put on the planet’s surface [3].
What is not established
Section titled “What is not established”The Viking sampler literature is a performance record, not an analysis. martin1977viking reports what the sampler did sol by sol but tabulates almost none of the underlying engineering numbers, force, torque, boom deflection, in extractable form, and its account of the sol 2 boom jamming is the design team’s reconstruction from telemetry and a matching ground failure rather than a reproduced fault [9]. The soil mechanics properties derived from the sampler and the rest of the lander were never measured directly by any instrument; Moore et al. state plainly that there is no sensible way to determine undisturbed drift density, that the widely quoted 1200 kg/m³ figure is only as good an estimate as any other, and that the anomalously low 18 degree friction angle for drift material has no settled explanation among pore-pressure, mixed shear failure and buried-obstruction hypotheses [11]. Both landing sites were in the northern plains, and Lander 2’s footpads both struck rocks, so no footpad penetration property exists for that site, and no rock strength was measured anywhere because nothing the sampler carried was built to chip or scratch rock [11]. Seger’s pre-launch account of the qualification program predates flight by two years and says only that component and subsystem testing was complete and the design appeared sound, without stating how well the flight units performed [12]. No source in this record ties a specific numeric fault tolerance or design margin to the sampler’s mechanisms; the anomaly record is a narrative of what sequence changes fixed each no-go, not an engineering post-mortem with root-cause margins attached.
References
- Siddiqi, A. A. (2018). Beyond Earth: A Chronicle of Deep Space Exploration, 1958-2016
. NASA, NASA SP-2018-4041. Source
BibTeX
@book{siddiqi2018beyond, title = {Beyond Earth: A Chronicle of Deep Space Exploration, 1958-2016}, author = {Siddiqi, Asif A.}, number = {NASA SP-2018-4041}, publisher = {NASA}, year = {2018}, url = {https://www.nasa.gov/wp-content/uploads/2018/09/beyond-earth-tagged.pdf} } - Smith, R. E. and West, G. S. (1983). Space and Planetary Environment Criteria Guidelines for Use in Space Vehicle Development, 1982 Revision (Volume 1)
. George C. Marshall Space Flight Center, NASA TM-82478. Source
BibTeX
@techreport{smith1983space, title = {Space and Planetary Environment Criteria Guidelines for Use in Space Vehicle Development, 1982 Revision (Volume 1)}, author = {Smith, Robert E. and West, George S.}, number = {NASA TM-82478}, institution = {George C. Marshall Space Flight Center}, year = {1983}, url = {https://ntrs.nasa.gov/citations/19830010545}, abstract = {Guidelines on space and planetary environment criteria for use in space vehicle development are provided. Information is incorporated in the disciplinary areas of atmospheric and ionospheric properties, radiation, geomagnetic field, astrodynamic constants, and meteoroids for the Earth's atmosphere above 90 km, interplanetary space, and the atmosphere and surfaces (when available) of the Moon and the planets (other than Earth) of this solar system. The Sun, Terrestrial Space, the Moon, Mercury, Venus, and Mars are covered.} } - Zacny, K., Paulsen, G., McKay, C. P., Glass, B., Davé, A., Dávila, A. F., Marinova, M., Mellerowicz, B., Heldmann, J. L., Stoker, C., Cabrol, N. A., Hedlund, M. and Craft, J. (2013). Reaching 1 m Deep on Mars: The Icebreaker Drill
. Astrobiology. Source
BibTeX
@article{zacny2013reaching, title = {Reaching 1 m Deep on Mars: The Icebreaker Drill}, author = {Zacny, K. and Paulsen, G. and McKay, Christopher P. and Glass, B. and Davé, A. and Dávila, Alfonso F. and Marinova, Margarita and Mellerowicz, B. and Heldmann, J. L. and Stoker, C. and Cabrol, Nathalie A. and Hedlund, Magnus and Craft, J.}, journal = {Astrobiology}, volume = {13}, pages = {1166-1198}, year = {2013}, doi = {10.1089/ast.2013.1038}, abstract = {The future exploration of Mars will require access to the subsurface, along with acquisition of samples for scientific analysis and ground-truthing of water ice and mineral reserves for in situ resource utilization. The Icebreaker drill is an integral part of the Icebreaker mission concept to search for life in ice-rich regions on Mars. Since the mission targets Mars Special Regions as defined by the Committee on Space Research (COSPAR), the drill has to meet the appropriate cleanliness standards as requested by NASA's Planetary Protection Office. In addition, the Icebreaker mission carries life-detection instruments; and in turn, the drill and sample delivery system have to meet stringent contamination requirements to prevent false positives. This paper reports on the development and testing of the Icebreaker drill, a 1 m class rotary-percussive drill and triple redundant sample delivery system. The drill acquires subsurface samples in short, approximately 10 cm bites, which makes the sampling system robust and prevents thawing and phase changes in the target materials. Autonomous drilling, sample acquisition, and sample transfer have been successfully demonstrated in Mars analog environments in the Arctic and the Antarctic Dry Valleys, as well as in a Mars environmental chamber. In all environments, the drill has been shown to perform at the “1-1-100-100” level; that is, it drilled to 1 m depth in approximately 1 hour with less than 100 N weight on bit and approximately 100 W of power. The drilled substrate varied and included pure ice, ice-rich regolith with and without rocks and with and without 2% perchlorate, and whole rocks. The drill is currently at a Technology Readiness Level (TRL) of 5. The next-generation Icebreaker drill weighs 10 kg, which is representative of the flightlike model at TRL 5/6. Key Words: Drilling—Sampling—Mars—Mars drilling—Subsurface exploration—Ice—Search for life. Astrobiology 13, 1166–1198. Table of contents Abstract 1. Introduction 2. The Martian Near Subsurface: Experience from Past Missions 3. Considerations When Designing a Drill for Mars Surface Operations 3.1. Science drivers 3.2. Environmental drivers 3.3. Planetary protection drivers 3.4. Technology drivers 4. The Icebreaker Mars Drill 4.1. Drilling depth 4.2. Selecting the best drilling method 4.3. Sample type 4.4. Components of the Icebreaker drill 4.4.1. Deployment boom 4.4.2. Z-stage 4.4.3. Drill head 4.4.4. Drill auger 4.4.5. Drill bit 4.4.6. Brushing station 4.5. Drilling software 4.5.1. Mission-critical events 4.5.2. Mission-noncritical events 4.6. Drill as a science instrument 5. Sample Acquisition 6. Sample Delivery 6.1. Five-DOF sampling arm and a scoop 6.2. Pneumatic sample transfer 6.3. Three-DOF-DOF arm and drill 7. Icebreaker Drill Tests 7.1. Test environment 7.2. Testing in a Mars environmental chamber 7.3. Testing in Mars analog sites of Antarctica 8. Next-Generation Icebreaker: The Icebreaker2 Drill 9. Conclusions Acknowledgments Abbreviations References} } - Bonitz, R. G., Shiraishi, L., Robinson, M., Arvidson, R. E., Chu, P. C., Wilson, J. J., Davis, K. R., Paulsen, G., Kusack, A. G., Archer, D. and Smith, P. (2008). NASA Mars 2007 Phoenix Lander Robotic Arm and Icy Soil Acquisition Device
. Journal of Geophysical Research: Planets. Source
BibTeX
@article{bonitz2008nasa, title = {NASA Mars 2007 Phoenix Lander Robotic Arm and Icy Soil Acquisition Device}, author = {Bonitz, Robert G. and Shiraishi, Lori and Robinson, Matthew and Arvidson, Raymond E. and Chu, P. C. and Wilson, J. J. and Davis, K. R. and Paulsen, G. and Kusack, A. G. and Archer, Doug and Smith, Peter}, journal = {Journal of Geophysical Research: Planets}, volume = {113}, pages = {E00A01}, publisher = {American Geophysical Union (AGU)}, year = {2008}, doi = {10.1029/2007je003030}, abstract = {The primary purpose of the Mars 2007 Phoenix Lander Robotic Arm (RA) and associated Icy Soil Acquisition Device (ISAD) is to acquire samples of Martian dry and icy soil (DIS) by digging, scraping, and rasping, and delivering them to the Thermal Evolved Gas Analyzer and the Microscopy, Electrochemistry, and Conductivity Analyzer. The RA will also position (1) the Thermal and Electrical Conductivity Probe (TECP) in the DIS; (2) the TECP at various heights above the surface for relative humidity measurements, and (3) the Robotic Arm Camera to take images of the surface, trench, DIS samples within the ISAD scoop, magnetic targets, and other objects of scientific interest within its workspace. The RA/ISAD will also be used to generate DIS piles for monitoring; conduct DIS scraping, penetration, rasping, and chopping experiments; perform compaction tests; and conduct trench cave‐in experiments. Data from the soil mechanics experiments will yield information on Martian DIS properties such as angle of repose, cohesion, bearing strength, and grain size distribution.} } - Bonitz, R., Shiraishi, L., Robinson, M., Carsten, J., Volpe, R., Trebi-Ollennu, A., Arvidson, R. E., Chu, P. C., Wilson, J. J. and Davis, K. R. (2009). The Phoenix Mars Lander Robotic Arm
. IEEE Aerospace Conference. Source
BibTeX
@inproceedings{bonitz2009phoenix, title = {The Phoenix Mars Lander Robotic Arm}, author = {Bonitz, Robert and Shiraishi, Lori and Robinson, Matthew and Carsten, Joseph and Volpe, Richard and Trebi-Ollennu, Ashitey and Arvidson, Raymond E. and Chu, P. C. and Wilson, J. J. and Davis, K. R.}, booktitle = {IEEE Aerospace Conference}, pages = {1-12}, organization = {Jet Propulsion Laboratory, California Institute of Technology}, address = {Big Sky, Montana}, year = {2009}, doi = {10.1109/aero.2009.4839306}, abstract = {The Phoenix Mars Lander Robotic Arm (RA) has operated for 149 sols since the Lander touched down on the north polar region of Mars on May 25, 2008. During its mission it has dug numerous trenches in the Martian regolith, acquired samples of Martian dry and icy soil, and delivered them to the Thermal Evolved Gas Analyzer (TEGA) and the Microscopy, Electrochemistry, and Conductivity Analyzer (MECA). The RA inserted the Thermal and Electrical Conductivity Probe (TECP) into the Martian regolith and positioned it at various heights above the surface for relative humidity measurements. The RA was used to point the Robotic Arm Camera to take images of the surface, trenches, samples within the scoop, and other objects of scientific interest within its workspace. Data from the RA sensors during trenching, scraping, and trench cave-in experiments have been used to infer mechanical properties of the Martian soil. This paper describes the design and operations of the RA as a critical component of the Phoenix Mars Lander necessary to achieve the scientific goals of the mission.} } - Okon, A. B. (2010). Mars Science Laboratory Drill
. Aerospace Mechanisms Symposium. Source
BibTeX
@inproceedings{okon2010mars, title = {Mars Science Laboratory Drill}, author = {Okon, Avi B.}, booktitle = {Aerospace Mechanisms Symposium}, address = {Cocoa Beach, Florida}, year = {2010}, url = {https://ntrs.nasa.gov/citations/20100021931}, abstract = {The Drill for the Mars Science Laboratory mission is a rotary-percussive sample acquisition device with an emphasis on toughness and robustness to handle the harsh environment on Mars. The unique challenges associated with autonomous drilling from a mobile robot are addressed. A highly compressed development schedule dictated a modular design architecture that satisfies the functional and load requirements while allowing independent development and testing of the Drill subassemblies. The Drill consists of four actuated mechanisms: a spindle that rotates the bit, a chuck that releases and engages bits, a novel voice-coil-based percussion mechanism that hammers the bit, and a linear translation mechanism. The Drill has three passive mechanisms: a replaceable bit assembly that acquires and collects sample, a contact sensor / stabilizer mechanism, and, lastly a flex harness service loop. This paper describes the various mechanisms that makeup the Drill and discusses the solutions to their unique design and development challenges.} } - Robinson, M., Collins, C., Leger, P., Carsten, J., Tompkins, V., Hartman, F. and Yen, J. (2013). In-Situ Operations and Planning for the Mars Science Laboratory Robotic Arm: The First 200 Sols
. IEEE International Conference on Systems, Man and Cybernetics. Source
BibTeX
@inproceedings{robinson2013situ, title = {In-Situ Operations and Planning for the Mars Science Laboratory Robotic Arm: The First 200 Sols}, author = {Robinson, Matthew and Collins, Curtis and Leger, Paul and Carsten, Joseph and Tompkins, Vandana and Hartman, Frank and Yen, Jeng}, booktitle = {IEEE International Conference on Systems, Man and Cybernetics}, volume = {tbd}, pages = {153-158}, year = {2013}, doi = {10.1109/sysose.2013.6575259}, abstract = {The Robotic Arm (RA) has operated for more than 200 Martian solar days (or sols) since the Mars Science Laboratory rover touched down in Gale Crater on August 5, 2012. During the first seven months on Mars the robotic arm has performed multiple contact science sols including the positioning of the Alpha Particle X-Ray Spectrometer (APXS) and/or Mars Hand Lens Imager (MAHLI) with respect to rocks or loose regolith targets. The RA has supported sample acquisition using both the scoop and drill, sample processing with CHIMRA (Collection and Handling for In- Situ Martian Rock Analysis), and delivery of sample portions to the observation tray, and the SAM (Sample Analysis at Mars) and CHEMIN (Chemistry and Mineralogy) science instruments. This paper describes the planning and execution of robotic arm activities during surface operations, and reviews robotic arm performance results from Mars to date.} } - Ezell, E. C. and Ezell, L. N. (1984). On Mars: Exploration of the Red Planet, 1958-1978
. NASA, NASA SP-4212. Source
BibTeX
@book{ezell1984mars, title = {On Mars: Exploration of the Red Planet, 1958-1978}, author = {Ezell, Edward Clinton and Ezell, Linda Neuman}, number = {NASA SP-4212}, publisher = {NASA}, year = {1984}, url = {https://ntrs.nasa.gov/citations/19840027188}, abstract = {The following aspects of the planet Mars were assessed directly and indirectly by the Viking lander and Viking orbiter spacecraft: the atmosphere, craters, volcanoes, terrain, geology, and evolution. Descriptions of these aspects are included herein. It is concluded that though life is certainly not abundant on Mars, the possibility still exists that some form of life is extant there.} } - Ezell, E. C. and Ezell, L. N. (1984). Viking Lander: Building a Complex Spacecraft
. On Mars: Exploration of the Red Planet, -, NASA SP-4212, NASA-SP-4212. Source
BibTeX
@incollection{ezell1984viking, title = {Viking Lander: Building a Complex Spacecraft}, author = {Ezell, Edward Clinton and Ezell, Linda Neuman}, booktitle = {On Mars: Exploration of the Red Planet, -, NASA SP-4212}, number = {NASA-SP-4212}, publisher = {NASA}, year = {1984}, url = {https://ntrs.nasa.gov/citations/19840027185}, abstract = {Various aspects of the design, testing, and preparation of the Viking lander spacecraft for Mars exploration are considered. The mission profile is given, including the entry into the Martian atmosphere and landing on the planet's surface. The return of scientific data to Earth is discussed. The top ten problem areas in the Viking lander project are enumerated, as are project costs. Pre-launch performance tests and preparation procedures are also addressed.} } - Martin Marietta Corporation. (1977). Viking 75 Project: Viking Lander System Primary Mission Performance Report
. NASA, NASA CR-145148. Source
BibTeX
@techreport{martin1977viking, title = {Viking 75 Project: Viking Lander System Primary Mission Performance Report}, author = {{Martin Marietta Corporation}}, number = {NASA CR-145148}, institution = {NASA}, year = {1977}, url = {https://ntrs.nasa.gov/citations/19770022101}, abstract = {Viking Lander hardware performance during launch, interplanetary cruise, Mars orbit insertion, preseparation, separation through landing, and the primary landed mission, with primary emphasis on Lander engineering and science hardware operations, the as-flown mission are described with respect to Lander system performance and anomalies during the various mission phases. The extended mission and predicted Lander performance is discussed along with a summary of Viking goals, mission plans, and description of the Lander, and its subsystem definitions.} } - Moore, H. J., Hutton, R. E., Clow, G. D. and Spitzer, C. R. (1987). Physical Properties of the Surface Materials at the Viking Landing Sites on Mars
. U.S. Geological Survey, Professional Paper 1389. Source
BibTeX
@techreport{moore1987physical, title = {Physical Properties of the Surface Materials at the Viking Landing Sites on Mars}, author = {Moore, Henry J. and Hutton, Robert E. and Clow, Gary D. and Spitzer, Cary R.}, number = {Professional Paper 1389}, institution = {U.S. Geological Survey}, year = {1987}, doi = {10.3133/pp1389}, abstract = {Estimates of water and carbon dioxide in samples analyzed in_ the gas chromatograph-mass spectrometer for the Molecular Analysis Experiment-----------------------} } - Seger, R. B. and Gillespie, V. P. (1973). The Viking Surface Sampler
. NASA Langley Research Center conference proceedings, paper 20. Source
BibTeX
@inproceedings{seger1973viking, title = {The Viking Surface Sampler}, author = {Seger, Robert B. and Gillespie, Vernon P.}, booktitle = {NASA Langley Research Center conference proceedings, paper 20}, pages = {245--255}, institution = {Martin Marietta Aerospace and NASA Langley Research Center}, year = {1973}, url = {https://ntrs.nasa.gov/citations/19740003574}, abstract = {A surface sampler subsystem for the Viking Lander has been designed, fabricated, cleaned, and successfully tested. Testing has included component level tests to qualification environment and subsystem level tests. This development hardware has also been integrated into a System Test Bed (STB) for the lander system. In addition to the normal dynamic and thermal environments the surface sampler hardware has been tested in an aircraft to simulate the effects of the reduced Martian gravity. Although problems have been encountered with the first-build and integration, the basic design appears to be sound and hardware qualification is scheduled for late 1973.} } - (2017). NASA Science: Viking 1. science.nasa.gov/mission/viking-1
BibTeX
@misc{nasascienceviking, title = {NASA Science: Viking 1}, organization = {science.nasa.gov}, year = {2017}, url = {https://science.nasa.gov/mission/viking-1/} }