Stardust was a 390-kilogram robotic space probe launched by NASA on 7 February 1999. Its primary mission was to collect dust samples from the coma of comet Wild2, as well as samples of cosmic dust, and return them to Earth for analysis. It was the first sample return mission of its kind. En route to comet Wild2, it also flew by and studied the asteroid 5535 Annefrank. The primary mission was successfully completed on 15 January 2006 when the sample return capsule returned to Earth.[9]
Fourth mission of the Discovery program; sample return from the periodic comet Wild 2
A mission extension, codenamed NExT, culminated in February 2011 with Stardust intercepting comet Tempel 1, a small Solar System body previously visited by DeepImpact in 2005. Stardust ceased operations in March 2011.
On 14 August 2014, scientists announced the identification of possible interstellar dust particles from the Stardust capsule returned to Earth in 2006.[10][11][12][13]
Mission background
History
Beginning in the 1980s, scientists began seeking a dedicated mission to study a comet. During the early 1990s, several missions to study comet Halley became the first successful missions to return close-up data. However, the US cometary mission, Comet Rendezvous Asteroid Flyby, was canceled for budgetary reasons. In the mid-1990s, further support was given to a cheaper, Discovery-class mission that would study comet Wild2 in 2004.[1]
Stardust was competitively selected in the fall of 1995 as a NASA Discovery Program mission of low-cost with highly focused science goals.[1]:5 Construction of Stardust began in 1996, and was subject to the maximum contamination restriction, level5 planetary protection. However, the risk of interplanetary contamination by alien life was judged low,[14] as particle impacts at over 1,000miles per hour, even into aerogel, were believed to be terminal for any known microorganism.[1]:22–23
Comet Wild2 was selected as the primary target of the mission for the rare chance to observe a long-period comet that has ventured close to the Sun. The comet has since become a short period comet after an event in 1974, where the orbit of Wild2 was affected by the gravitational pull of Jupiter, moving the orbit inward, closer to the Sun. In planning the mission, it was expected that most of the original material from which the comet formed would still be preserved.[1]:5
The primary science objectives of the mission included:[6]
Providing a flyby of a comet of interest (Wild2) at a sufficiently low velocity (less than 6.5km/s) such that non-destructive capture of comet dust is possible using an aerogel collector.
Facilitating the intercept of significant numbers of interstellar dust particles using the same collection medium, also at as low a velocity as possible.
Returning as many high-resolution images of the comet coma and nucleus as possible, subject to the cost constraints of the mission.
The spacecraft was designed, built and operated by Lockheed Martin Astronautics as a Discovery-class mission in Denver, Colorado. JPL provided mission management for the NASA division for mission operations. The principal investigator of the mission was Dr.Donald Brownlee from the University of Washington.[1]:5
Spacecraft design
The spacecraft bus measured 1.7 meters (5ft 7in) in length, and 0.66 meters (2ft 2in) in width, a design adapted from the SpaceProbe deep space bus developed by Lockheed Martin Astronautics. The bus was primarily constructed with graphite fiber panels with an aluminum honeycomb support structure underneath; the entire spacecraft was covered with polycyanate, Kapton sheeting for further protection. To maintain low costs, the spacecraft incorporated many designs and technologies used in past missions or previously developed for future missions by the Small Spacecraft Technologies Initiative (SSTI). The spacecraft featured five scientific instruments to collect data, including the Stardust Sample Collection tray, which was brought back to Earth for analysis.[15]
Attitude control and propulsion
The spacecraft was three-axis stabilized with eight 4.41N hydrazine monopropellant thrusters, and eight 1-Newton thrusters to maintain attitude control (orientation); necessary minor propulsion maneuvers were performed by these thrusters as well. The spacecraft was launched with 80kilograms of propellant. Information for spacecraft positioning was provided by a star camera using FSW to determine attitude (stellar compass), an inertial measurement unit, and two sun sensors.[1]:30–31[15]
Communications
For communicating with the Deep Space Network, the spacecraft transmitted data across the X-band using a 0.6-meter (2ft 0in) parabolic high-gain antenna, medium-gain antenna (MGA) and low-gain antennas (LGA) depending on mission phase, and a 15-watt transponder design originally intended for the Cassini spacecraft.[1]:32[15]
Power
The probe was powered by two solar arrays, providing an average of 330watts of power. The arrays also included Whipple shields to protect the delicate surfaces from the potentially damaging cometary dust while the spacecraft was in the coma of Wild2. The solar array design was derived primarily from the Small Spacecraft Technology Initiative (SSTI) spacecraft development guidelines. The arrays provided a unique method of switching strings from series to parallel depending on the distance from the Sun. A single nickel–hydrogen (NiH2) battery was also included to provide the spacecraft with power when the solar arrays received too little sunlight.[1]:31[15]
Computer
The computer on the spacecraft operated using a radiation-hardened RAD6000 32-bit processor card. For storing data when the spacecraft was unable to communicate with Earth, the processor card was able to store 128megabytes, 20% of which was occupied by the flight system software. The system software is a form of VxWorks, an embedded operating system developed by Wind River Systems.[1]:31[15]
Scientific instruments
Navigation Camera (NC)
The camera is intended for targeting comet Wild2 during the flyby of the nucleus. It captures black and white images through a filter wheel making it possible to assemble color images and detect certain gas and dust emissions in the coma. It also captures images at various phase angles, making it possible to create a three-dimensional model of a target to better understand the origin, morphology, and mineralogical inhomogeneities on the surface of the nucleus. The camera utilizes the optical assembly from the Voyager Wide Angle Camera. It is additionally fitted with a scanning mirror to vary the viewing angle and avoid potentially damaging particles. For environmental testing and verification of the NAVCAM the only remaining Voyager spare camera assembly was used as a collimator for testing of the primary imaging optics. A target at the focal point of the spare was imaged through the optical path of the NAVCAM for verification.[16][17]
The dust analyzer is a mass spectrometer able to provide real-time detection and analysis of certain compounds and elements. Particles enter the instrument after colliding with a silver impact plate and traveling down a tube to the detector. The detector is then able to detect the mass of separate ions by measuring the time taken for each ion to enter and travel through the instrument. Identical instruments were also included on Giotto and Vega1 and2.[18][19]
Located on the Whipple shield at the front of the spacecraft, the sensor unit provides data regarding the flux and size distribution of particles in the environment around Wild2. It records data by generating electric pulses as a special polarized plastic (PVDF) sensor is struck by high energy particles as small as a few micrometers.[20][21]
The particle collector uses aerogel, a low-density, inert, microporous, silica-based substance, to capture dust grains as the spacecraft passes through the coma of Wild2. After sample collection was complete, the collector receded into the Sample Return Capsule for entering the Earth's atmosphere. The capsule with encased samples would be retrieved from Earth's surface and studied.[22][23]
Determine the elemental, chemical, and mineralogical composition of Wild2 at the submicron scale.
Determine which compounds dominate the organic fraction of Wild2.
Establish the building materials of Wild2 found in interplanetary dust particles (IDP) and meteorites.
Determine the extent of the building materials of Wild2 found in interplanetary dust particles (IDP) and meteorites.
Establish if IDPs are consistent with Wild2 samples.
Determine if pyroxenerich chondritic aggregate IDPs are cometary.
Establish if amino acids, quinones, amphiphiles, or other molecules of exobiological interest are present.
Determine the state of H2O in Wild2.
Determine if there was mixing of inner nebula materials (i.e., high-temperature condensates) in the region of comet formation in the outer nebula.
Characterize isotopic anomalies present which could provide signatures of the place of origin of interstellar grains
Determine the high deuterium-to-hydrogen ratios seen in some IDPs common in Wild2 solids
Characterize the nature of the carbonaceous material in Wild2, and the relationship to silicates and other mineral phases or constraints in the processes by which they were formed (ion-molecule, gas-grain, irradiation of ices, etc.)
Determine if there are organic refractory mantles on silicate grains and if they resemble the organics found in IDPs and meteorites
Provide evidence of preaccretional processing of grains (cosmic ray tracks, sputtered rims, altered mineralogy, etc.)
Determine if GEMS (Glass with Embedded FeNi Metal and Sulfides) are present
Principal investigator: Donald Brownlee / University of Washington
The experiment will primarily utilize the X band telecommunications system to conduct radio science on Wild2, to determine the mass of the comet; secondarily the inertial measurement unit is utilized to estimate the impact of large particle collisions on the spacecraft.[24][25]
Determine the mass and bulk density of comet Wild2.
Determine the coma density and constrain the particle size distribution for comet Wild2.
Sound the solar corona at Xband, including electron content of the inner corona, solar wind acceleration, turbulence, and a search for coronal mass ejections.
Comet and interstellar particles are collected in ultra low density aerogel. The tennis racket-sized collector tray contained ninety blocks of aerogel, providing more than 1,000square centimeters of surface area to capture cometary and interstellar dust grains.
To collect the particles without damaging them, a silicon-based solid with a porous, sponge-like structure is used in which 99.8percent of the volume is empty space. Aerogel has 1⁄1000the density of glass, another silicon-based solid to which it may be compared. When a particle hits the aerogel, it becomes buried in the material, creating a long track, up to 200times the length of the grain. The aerogel was packed in an aluminium grid and fitted into a Sample Return Capsule (SRC), which was to be released from the spacecraft as it passed Earth in 2006.
To analyze the aerogel for interstellar dust, one million photographs will be needed to image the entirety of the sampled grains. The images will be distributed to home computer users to aid in the study of the data using a program titled, Stardust@home. In April 2014, NASA reported they had recovered seven particles of interstellar dust from the aerogel.[26]
Images of the spacecraft
Diagram of the spacecraft
Stardust capsule with aerogel collector deployed
Stardust awaiting testing of the solar arrays
The solar arrays being checked in the Payload Hazardous Servicing Facility
Stardust being checked before encapsulation
Stardust microchip
Stardust was launched carrying two sets of identical pairs of square 10.16-centimeter (4in) silicon wafers. Each pair featured engravings of well over one million names of people who participated in the public outreach program by filling out internet forms available in late 1997 and mid-1998. One pair of the microchips was positioned on the spacecraft and the other was attached to the sample return capsule.[1]:24
Stardust was launched at 21:04:15UTC on 7 February 1999, by the National Aeronautics and Space Administration from Space Launch Complex17A at the Cape Canaveral Air Force Station in Florida, aboard a DeltaII 7426 launch vehicle. The complete burn sequence lasted for 27minutes bringing the spacecraft into a heliocentric orbit that would bring the spacecraft around the Sun and past Earth for a gravity assist maneuver in 2001, to reach asteroid 5535 Annefrank in 2002 and comet Wild2 in 2004 at a low flyby velocity of 6.1km/s. In 2004, the spacecraft performed a course correction that would allow it to pass by Earth a second time in 2006, to release the Sample Return Capsule for a landing in Utah in the Bonneville Salt Flats.[1]:14–22[6]
During the second encounter with Earth, the Sample Return Capsule was released on Jan 15, 2006.[6] Immediately afterwards, Stardust was put into a "divert maneuver" to avoid entering the atmosphere alongside the capsule. Under twenty kilograms of propellant remained onboard after the maneuver.[6] On 29 January 2006, the spacecraft was put in hibernation mode with only the solar panels and receiver active, in a 3-year heliocentric orbit that would return it to Earth vicinity on 14 January 2009.[6][27]
A subsequent mission extension was approved on 3 July 2007, to bring the spacecraft back to full operation for a flyby of comet Tempel1 in 2011. The mission extension was the first to revisit a small Solar System body and used the remaining propellant, signaling the end of the useful life for the spacecraft.[28]
At 04:50:20UTC on 2 November 2002, Stardust encountered asteroid 5535Annefrank from a distance of 3,079km (1,913mi).[6] The solar phase angle ranged from 130degrees to 47degrees during the period of observations. This encounter was used primarily as an engineering test of the spacecraft and ground operations in preparation for the encounter with comet Wild2 in 2003.[6]
Image of asteroid Annefrank captured on 2 November 2002
False-color image of asteroid Annefrank
Encounter with Wild 2
At 19:21:28UTC, on 2 January 2004, Stardust encountered Comet Wild2[33] on the sunward side with a relative velocity of 6.1km/s at a distance of 237km (147mi).[6] The original encounter distance was planned to be 150km (93mi), but this was changed after a safety review board increased the closest approach distance to minimize the potential for catastrophic dust collisions.[6]
The relative velocity between the comet and the spacecraft was such that the comet actually overtook the spacecraft from behind as they traveled around the Sun. During the encounter, the spacecraft was on the Sunlit side of the nucleus, approaching at a solar phase angle of 70degrees, reaching a minimum angle of 3degrees near closest approach and departing at a phase angle of 110degrees.[6] The AutoNav software was used during the flyby.[34]:11
During the flyby the spacecraft deployed the Sample Collection plate to collect dust grain samples from the coma, and took detailed pictures of the icy nucleus.[35]
Comet Wild2 as seen from Stardust on 2 January 2004
Image of Wild2 taken during the closest approach phase
An overexposed image of Wild2 showing plumes of material
A 3D anaglyph of comet Wild2
New Exploration of Tempel 1 (NExT)
Artist's impression of the Stardust spacecraft performing a burn-to-depletion at the end of the Stardust NExT mission.
On 19 March 2006, Stardust scientists announced that they were considering the possibility of redirecting the spacecraft on a secondary mission to image Comet Tempel1. The comet was previously the target of the DeepImpact mission in 2005, sending an impactor into the surface. The possibility of this extension could be vital for gathering images of the impact crater which Deep Impact was unsuccessful in capturing due to dust from the impact obscuring the surface.
On 3 July 2007 the mission extension was approved and renamed New Exploration of Tempel1 (NExT). This investigation would provide the first look at the changes to a comet nucleus produced after a close approach to the Sun. NExT also would extend the mapping of Tempel1, making it the most mapped comet nucleus to date. This mapping would help address the major questions of comet nucleus geology. The flyby mission was expected to consume almost all of the remaining fuel, signaling the end of the operability of the spacecraft.[28] The AutoNav software (for autonomous navigation) would control the spacecraft for the 30 minutes prior to encounter.[36]
The mission objectives included the following:[36]
Primary objectives
Extend the current understanding of the processes that affect the surfaces of comet nuclei by documenting the changes that have occurred on comet Tempel1 between two successive perihelion passages, or orbits around the Sun.
Extend the geologic mapping of the nucleus of Tempel1 to elucidate the extent and nature of layering, and help refine models of the formation and structure of comet nuclei.
Extend the study of smooth flow deposits, active areas and known exposure of water ice.
Secondary objectives
Potentially image and characterize the crater produced by Deep Impact in July 2005, to better understand the structure and mechanical properties of cometary nuclei and elucidate crater formation processes on them.
Measure the density and mass distribution of dust particles within the coma using the Dust Flux Monitor Instrument.
Analyze the composition of dust particles within the coma using the Comet and Interstellar Dust Analyzer instrument.
Encounter with Tempel 1
Main article: 9P/Tempel
At 04:39:10UTC on 15 February 2011, Stardust-NExT encountered Tempel1 from a distance of 181km (112mi).[7][8] An estimated 72images were acquired during the encounter. These showed changes in the terrain and revealed portions of the comet never seen by Deep Impact.[37] The impact site from Deep Impact was also observed, though it was barely visible due to material settling back into the crater.[38]
Tempel1 from the Stardust-NExT spacecraft during closest approach
'Before and after' comparison images of Tempel1 by DeepImpact (left) and Stardust (right)
End of extended mission
On 24 March 2011 at approximately 23:00UTC, Stardust conducted a burn to consume its remaining fuel.[32] The spacecraft had little fuel left and scientists hoped the data collected would help in the development of a more accurate system for estimating fuel levels on spacecraft. After the data had been collected, no further antenna aiming was possible and the transmitter was switched off. The spacecraft sent an acknowledgement from approximately 312millionkm (194millionmi) away in space.[4]
Sample return
Landing capsule as seen by the recovery team
On 15 January 2006, at 05:57UTC, the Sample Return Capsule successfully separated from Stardust. The SRC re-entered the Earth's atmosphere at 09:57UTC,[39] with a velocity of 12.9km/s, the fastest reentry speed into Earth's atmosphere ever achieved by a human-made object.[40] The capsule followed a drastic reentry profile, going from a velocity of Mach36 to subsonic speed within 110 seconds.[41][failed verification] Peak deceleration was 34g,[42] encountered 40seconds into the reentry at an altitude of 55km over Spring Creek, Nevada.[41] The phenolic-impregnated carbon ablator (PICA) heat shield, produced by Fiber Materials Inc., reached a temperature of more than 2,900°C during this steep reentry.[43] The capsule then parachuted to the ground, finally landing at 10:12UTC at the Utah Test and Training Range, near the U.S.Army Dugway Proving Ground.[5][44] The capsule was then transported by military aircraft from Utah to Ellington Air Force Base in Houston, Texas, then transferred by road in an unannounced convoy to the Planetary Materials Curatorial facility at Johnson Space Center in Houston to begin analysis.[6][45]
Sample processing
Visible dust grains in the aerogel collector
The sample container was taken to a clean room with a cleanliness factor 100times that of a hospital operating room to ensure the interstellar and comet dust was not contaminated.[46] Preliminary estimations suggested at least a millionmicroscopic specks of dust were embedded in the aerogel collector. Tenparticles were found to be at least 100micrometers (0.1mm) and the largest approximately 1,000micrometers (1mm). An estimated 45interstellar dust impacts were also found on the sample collector, which resided on the back side of the cometary dust collector. Dust grains are being observed and analyzed by a volunteer team through the citizen science project, Stardust@Home.
The combined mass of the harvested sample was approximately 1 mg.[47]
In December 2006, seven papers were published in the scientific journal Science, discussing initial details of the sample analysis. Among the findings are: a wide range of organic compounds, including two that contain biologically usable nitrogen; indigenous aliphatic hydrocarbons with longer chain lengths than those observed in the diffuse interstellar medium; abundant amorphous silicates in addition to crystalline silicates such as olivine and pyroxene, proving consistency with the mixing of Solar System and interstellar matter, previously deduced spectroscopically from ground observations;[48] hydrous silicates and carbonate minerals were found to be absent, suggesting a lack of aqueous processing of the cometary dust; limited pure carbon (CHON)[clarification needed] was also found in the samples returned; methylamine and ethylamine was found in the aerogel but was not associated with specific particles.
In 2010, Dr. Andrew Westphal announced that Stardust@home volunteer Bruce Hudson found a track (labeled "I1043,1,30") among the many images of the aerogel that may contain an interstellar dust grain.[49] The program allows for any volunteer discoveries to be recognized and named by the volunteer. Hudson named his discovery "Orion".[50]
Stardust@Home certificate
In April 2011, scientists from the University of Arizona discovered evidence for the presence of liquid water in comet Wild 2. They have found iron and copper sulfide minerals that must have formed in the presence of water. The discovery shatters the existing paradigm that comets never get warm enough to melt their icy bulk.[51] In the spring of 2014, the recovery of particles of interstellar dust from the Discovery program's Stardust mission was announced.[52]
The Stardust samples are currently available for everyone to identify after completing the training at Berkeley webpage.[53]
Spacecraft location
The return capsule is currently located at the National Air and Space Museum in Washington, D.C. It began exhibition there on 1 October 2008, the 50th anniversary of the establishment of NASA. The return capsule is displayed in sample collection mode, alongside a sample of the aerogel used to collect samples.[54]
Results
The comet samples show that the outer regions of the early Solar System were not isolated and were not a refuge where interstellar materials could commonly survive.[55] The data suggest that high-temperature inner Solar System material formed and was subsequently transferred to the Kuiper belt.[56]
Glycine
In 2009 it was announced by NASA that scientists had identified one of the fundamental chemical building blocks of life in a comet for the first time: glycine, an amino acid, was detected in the material ejected from comet Wild2 in 2004 and captured by the Stardust probe. Glycine has been detected in meteorites before and there are also observations in interstellar gas clouds, but the Stardust find is described as a first in cometary material. Isotope analysis indicates that the Late Heavy Bombardment included cometary impacts after the Earth coalesced but before life evolved.[57] Carl Pilcher, who leads NASA's Astrobiology Institute commented that "The discovery of glycine in a comet supports the idea that the fundamental building blocks of life are prevalent in space, and strengthens the argument that life in the universe may be common rather than rare."[58]
See also
Spaceflight portal
List of missions to comets
Genesis, sample return from the solar wind
Hayabusa, sample return from an asteroid
List of uncrewed spacecraft by program
Robotic spacecraft
Space exploration
Space probe
Timeline of artificial satellites and space probes
Timeline of first orbital launches by country
Timeline of Solar System exploration
References
"Stardust Launch"(PDF) (Press Kit). NASA. February 1999. Archived(PDF) from the original on 16 November 2001.
Newburn, R. L. Jr.; Bhaskaran, S.; Duxbury, T. C.; Fraschetti, G.; Radey, T.; Schwochert, M. (14 October 2003). "Stardust Imaging Camera". Journal of Geophysical Research. 108 (8116): 8116. Bibcode:2003JGRE..108.8116N. doi:10.1029/2003JE002081.
Gasner, Steve; Sharmit, Khaled; Stella, Paul; Craig, Calvin; Mumaw, Susan (2003). The Stardust solar array. 3rd World Conference on Photovoltaic Energy Conversion. 11–18 May 2003. Osaka, Japan.
Van Boekel, R.; Min, M.; Leinert, Ch.; Waters, L. B. F. M.; Richichi, A.; Chesneau, O.; Dominik, C.; Jaffe, W.; Dutrey, A.; Graser, U.; Henning, Th.; De Jong, J.; Köhler, R.; De Koter, A.; Lopez, B.; Malbet, F.; Morel, S.; Paresce, F.; Perrin, G.; Preibisch, Th.; Przygodda, F.; Schöller, M.; Wittkowski, M. (2004). "The building blocks of planets within the 'terrestrial' region of protoplanetary disks". Nature. 432 (7016): 479–82. Bibcode:2004Natur.432..479V. doi:10.1038/nature03088. PMID15565147. S2CID4362887.
Brownlee, Don (5 February 2014). "The Stardust Mission: Analyzing Samples from the Edge of the Solar System". Annual Review of Earth and Planetary Sciences. 42 (1): 179–205. Bibcode:2014AREPS..42..179B. doi:10.1146/annurev-earth-050212-124203.
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