Hayabusa arrived at its exploration target, near Earth asteroid Itokawa, on September 12th of this year after having been propelled there via ion engines and an Earth swing-by. Since then, it has successfully performed orbital manoeuvres, precisely keeping its position relative to Itokawa. The Hayabusa project team has made many discoveries while carrying out their ambitious scientific observations of Itokawa. This release summarizes and reports the major scientific and engineering achievements in advance of Hayabusa's unprecedented and historic descent to the surface of Itokawa for sample collection middle to later this month.
Itokawa +270 deg Surface
Itokawa +90 deg Surface
Hayabusa is a technology demonstration spacecraft focusing on key technologies that are required for future large-scale sample and return missions, yet is also making new scientific observations and discoveries. The technology demonstration component of the mission consists of five goals: ion engine propulsion in interplanetary cruise, ion engine propulsion in combination with an Earth gravity assist, autonomous guidance and navigation using optical measurements, collection of surface samples in an ultra-low gravity environment and the direct recovery of these samples on the ground after its return from interplanetary flight. To date the Hayabusa project has accomplished these demonstrations up through the third goal. Specifically, at the time of arrival at Itokawa, Hayabusa had driven its proprietary new ion engines for 26,000 hours, including their operation during an Earth flyby. It has also perfectly completed a period of hybrid optical navigation followed by precise guidance and navigation of the spacecraft during its station keeping period around Itokawa. These engineering achievements are the primary mission of Hayabusa and their successful completion is a great achievement.
The deep-space exploration technologies that the world's space agencies are pursuing consist of three major elements: high efficiency electric propulsion for cruise, rendezvous with target destinations and round-trip flights back to the Earth. As of this time Hayabusa has accomplished the first and second of these elements, leading the way for the space exploration agencies of the world. Furthermore, robotic sample collection and return from an extra terrestrial object has not been executed before, and is not currently planned, except for Hayabusa, which will attempt to gather a bulk sample from Itokawa. Hayabusa's success clearly shows that Japan's deep space exploration technology has reached the level of the world's most developed space agencies, and that Japan is now in a leadership position in some select engineering fields. Thus Hayabusa opens a new era in solar system exploration.
180 deg Surface
50 deg Surface
For the scientific aspects of the mission, Hayabusa carries four instruments that have performed successful observations to date: AMICA, a visible imager with multi-band filters has exposed 1,500 images amounting to almost 1 GB of data, NIRS, a near infrared spectrometer has taken 75,000 measurements distributed globally over the body, LIDAR, a laser altimeter has accumulated 1.4 million measurements globally, and XRS, a X-ray spectrometer has received and integrated its signal for 700 hours. In addition to these, spacecraft-tracking data has been used to measure properties of the asteroid as well. These unprecedented scientific measurements are briefly described and reported in what follows.
(A) Morphological and geological discoveries about Itokawa: The a priori theoretical assumption that small near-Earth asteroids should have geologically homogeneous features was completely overturned by the observation of a wide variety of surface features and types at Itokawa. The surface is covered with huge boulders and, for the first time, naked surfaces not covered with regolith have been exposed. Previously visited asteroids were covered with thick regolith, thus Itokawa's surface is like nothing that has seen before, which is quite fortunate for the Hayabusa mission. The opportunity to observe the true asteroid surface, which is usually concealed from view, advances our understanding of spectroscopic observations of asteroids taken from Earth, and allows us to expand our knowledge of near Earth asteroids.
(B) Taking advantage of the observations made with the onboard instruments, sufficiently detailed information about the sampling sites has been obtained, and the relation between the potential samples and the spectroscopic data has been correctly correlated. As a technology demonstration mission, Hayabusa has already finished the preliminary steps towards the primary sample and return goal. These samples will provide important scientific clues concerning the puzzlingly inconsistent correlations between S-type asteroids and ordinary chondrites, and lead to an improved understanding of the space weathering effect, which may clarify our understanding of the early solar system and Earth.
(C) Combinations of the Itokawa images along with spacecraft navigation information has enabled shape and gravity models to be numerically defined. The science team has started to study and identify the special mechanisms that can move boulders and regolith in the ultra-low gravity environment associated with small objects. The gravity and slope information and estimates of the density of boulders and regolith distribution on the surface, combined with comparisons with meteorites, will advance our interpretation and understanding of asteroid planetology.
(D) Using the laser altimeter and optical navigation camera, along with range and range-rate measurements from ground-tracking stations, have led to a successful mass and density estimate for Itokawa. The density has been estimated to be 2.3 +/-0.3 gram/cc, which is a little lower than that measured for rocks on the ground or for other S-type asteroids measured to date. This may indicate that there is substantial porosity for this body, and forces conventional views of these small objects to be changed drastically. When the samples are successfully returned and recovered, the actual porosity will be clarified and our knowledge of how the Earth relates to meteorites will be greatly improved.
Gravity and slope Map
The exploration of small solar system bodies contributes to an improved understanding of the Earth itself, as well as to a more comprehensive interpretation of the constituents and potential resources that these celestial objects contain. The scientific discoveries reported here will redefine scientific notions and views of asteroids from the pre-Hayabusa era, and are a remarkable accomplishment that Japan has contributed to planetary exploration.
In view of the scientific results described above, JAXA has determined the landing/sampling sites candidates and the descent target point for rehearsal, along with their planned dates and times. The landing/sampling sites must be free of obstacles and smooth enough to ensure safety, a top priority, while at the same time the surface inclination and the ground station coverage for Hayabusa must be taken into account. Taking these issues into consideration, the candidate sites and schedule were determined.
candidate-A
The first site candidate is the regolith expanse in the middle of Itokawa, known as the MUSES-SEA area , and the second candidate site is the Woomera desert at the tip end of Itokawa, where the terrain is broad and flat. The rehearsal target is the area located close to the spin axis, a little east of the first site. The date and time of the planned events (Japan Standard Time) are listed below.
The purpose of the rehearsal descent is, first of all, to make sure that the proximity laser range finder works as intended, as its function has not been calibrated during cruise. The second purpose is to confirm whether the target marker image can be extracted against the asteroid surface, using onboard image processing that illuminates it using flash lamps onboard the spacecraft. The third purpose is to deploy and place the hopping robot MINERVA on the asteroid surface. Deploying MINERVA conflicts with the touch-down sequence, so it will be separated in advance of the sampling runs.
Sampling Sites
In conjunction with this very big challenge, JAXA is also starting a nation-wide campaign called 'You Name the Landing Site'. The names assigned to the sites may not be officially registered by the International Astronomy Union (IAU) as the sites are very small. However, JAXA, as a finder, declares that the sites will be given those selected names. The application page is https://ssl.tksc.jaxa.jp/hayabusa/ and will be open until 17:00 on November 30th. The application form there is available from early November. The actual naming will occur after the completion of the Hayabusa proximity observation period, in early December.
The descent to the asteroids surface was aborted on November 4, 2005, due to a detection of anomalous signal at GO/NOGO decision. The descent, including release of MINERVA and the target marker has been cancelled.
This is an image of Itokawa obtained at around 11:40 am JST.
The Current Status of the Near-Infrared Spectrometer (NIRS)
The Hayabusa Near-Infrared Spectrometer (NIRS) is an instrument that obtains spectra of the sunlight reflected off the surface of asteroid Itokawa. The spectrograph decomposes the reflected sunlight into counts for individual wavelengths across a known spectral region. A spectrum shows the intensity of the light at each wavelength, and the change in intensity shows the colour of the material on the surface of the asteroid. By investigating the asteroid's colours at near-infrared wavelengths, we can understand the mineralogy of the surface.
This image shows the region of Hayabusa where NIRS observed between Sep. 16 and Oct. 12. Since NIRS observes a restricted, small area (the field of view is 0.1 x 0.1 degrees) during one observation, the investigation of the whole asteroid takes much time.
Until now, NIRS' observations have concentrated around the equatorial region of Itokawa. Observations of high latitude areas will be attempted when the spacecraft moves to a position where it will become easy to observe the North Pole and South Pole of Itokawa.
This image shows a data cloud of LIDAR measurements on the surface of the asteroid Itokawa. The data is plotted on model shape generated using ground-based radar observations taken before the arrival of HAYABUSA at Itokawa. As the HAYABUSA spacecraft is mostly located on the equatorial plane of Itokawa, the mission team has already obtained sufficient ranging data to model the asteroid’s equatorial shape. However, this is not the case at the poles, where few data points exist.
The LIght Detection And Ranging sensor (LIDAR) or laser altimeter measures the time for a single pulse of laser light to travel between the HAYABUSA spacecraft and the surface of Itokawa, and back. Knowing the speed of light, a distance between the spacecraft and asteroid surface can be determined. By combining such LIDAR ranging data and images obtained by the optical navigation camera, the navigation system on board of the HAYABUSA spacecraft can accurately estimate its position relative to the asteroid.
Hayabusa has arrived at the Home Position, (it actually arrived on September 30th) and is currently in a new flight phase. Hayabusa is taking high altitude images and inspecting potential landing sites. This phase will last one month.
The bad news is that the space probe has lost the use of two reaction wheels. One packed up on July 31st for the X-axis, and on October 2nd for the Y-axis. The altitude stabilisation is now being preformed by the one remaining wheel and the two RCS engines.
This image was taken from the Home Position , 7 Km, from the surface.
Hayabusa arrived at the Gate Position, about 20 km from Itokawa on September 12th. Since then to 21st, Hayabusa had kept the relative position control (Station Keeping) via the Optical Hybrid Navigation.
A three dimensional view of the trajectory as well as its time history is shown here.
The coordinate used here is, so called, HP (Home Position) frame, in which the Z axis is taken to the Earth direction and Y-axis is southward in ecliptic frame and normal to the plane that is spanned by Sun-to-Itokawa and Sun-to-Earth lines and X-axis should constitute the right-hand coordinate.
The station manoeuvres and maintains its altitude (Z-position) and at the same time controls the Itokawa direction at the centre in X-Y plane. The control box defined is a little loosened so that the number of corrections can be minimized. Even 1 cm/second velocity residual leads to the drift of up to 1 km per day, so the station keeping is performed very carefully.
Soon Hayabusa will lower its altitude to the Home Position, where this task will be much harder due to the high sensitivity.
The spacecraft employs an Optical Navigation Camera (ONC), a LIght Detection And Ranging (LIDAR), a Laser Range Finder (LRF) and Fan Beam Sensors (FBS) to gather topographic and range information about the asteroid's surface.
The spacecraft will approach and stay near the asteroid for about five months, with autonomous navigation and guidance using ONC and LIDAR. After constructing a 3D model of the asteroid while the two months of the global mapping phase, MUSES-C project team will decide a landing point considering some constraints.
To land upon and gather fragments from the surface of the asteroid, the spacecraft has optical autonomous navigation, guidance and control system, which employs ONC and LIDAR above 100m altitude. For the measurement of the relative position and attitude to the surface in the final landing phase under 100m altitude, ONC, LRF and a Target Marker (TM), which is an artificial target and released at about 100m altitude, are used. FBSs are also used for obstacle detection.
Touch down is detected by another LRF which measures the distance between LRF and the sampler horn and a bullet is fired. Just after sampling, the spacecraft will lift off immediately and autonomously re-establish three-axis attitude and safe position.
Hayabusa has been imaging and collecting spectral data from its "Gate Position" 20 kilometres from asteroid Itokawa.
The spacecraft is now moving, currently from 12 kilometres, to the "Home Position", just 7 kilometres distance.
Eventually, two surface sampling missions are scheduled for the second half of November.
"There are smooth regions and areas where several sizable surface chunks and boulders reside. Normally, one would expect these boulders to be caused by impacts but surprisingly, there are no obvious impact craters. As is usually the case with successful small-body missions, there is a whole new set of questions to answer" - Donald Yeomans, senior research scientist and asteroid expert at the Jet Propulsion Laboratory (JPL) in Pasadena, California.