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On Christmas Day 2004, the Cassini spacecraft flawlessly released ESA's Huygens probe, passing another challenging milestone for Cassini-Huygens mission. But, with no telemetry data from Huygens, how do we know the separation went well? At 3:00 CET on 25 December, the critical sequence loaded into the software on board Cassini was executed and, within a few seconds, Huygens was sent on its 20-day trip towards Titan. As data from Cassini confirm, the pyrotechnic devices were fired to release a set of three loaded springs, which gently pushed Huygens away from the mother spacecraft. The probe was expected to be released at a relative velocity of about 0.35 meters per second with a spin rate of about 7.5 revolutions per minute. Telemetry data from Cassini confirming the separation were collected by NASA's Deep Space Network stations in Madrid, Spain, and Goldstone, California, when the telemetry playback signal from Cassini eventually reached the Earth. However, these data showed only that the Cassini systems had worked, and that the Cassini 'attitude perturbation' (how Cassini moved in reaction to the probe's release) were as expected. Within hours, the preliminary analysis of this data confirmed that Huygens was on the expected trajectory and spinning within the expected range. The spin imparted to Huygens is vitally important to ensure that the probe remains in a stable attitude and on course when it enters Titan's atmosphere.
How do we know that it is on the right course and how accurately can we tell? Since Huygens has no propulsion system of its own, it had to be put on course for its descent before it was released. As planned, a fine tuning of the Cassini trajectory took place on 22 December to place Huygens on its nominal entry trajectory. While Huygens will remain on this trajectory until it plunges into Titan's atmosphere on 14 January, the Cassini orbiter performed a deflection maneuver on 28 December to avoid crashing onto the moon. Huygens is scheduled to reach Titan's upper atmosphere at about 10:06 CET (4:06 AM EST) on 14 January, entering the atmosphere at a relatively steep angle of 65° and a velocity of about six kilometers per second (>10,000 miles per hour). The fine-tuning maneuver, called 'Targeting Clean-up', was critical: if the entry angle is too steep, the probe could overheat and burn up in the atmosphere; if the angle is too shallow, the probe might skim like a pebble on the surface of a lake and miss its target. After the probe's separation from Cassini, telemetry data were collected by NASA's Deep Space Network stations in Madrid, Spain, and Goldstone, California. From these data confirming the release, we know the speed after release, and that the probe is spinning as planned to keep stable. Images from Cassini's cameras showing the probe drifting away were taken on 25-27 October.
Although only a few pixels across, these images taken at different distances between the probe and the orbiter helped navigators to reconstruct the probe's trajectory. Using the backdrop of known stars, and pinpointing Huygens's position relative to Cassini, the probe's trajectory was reconstructed using radio and optical navigation techniques. This information is important to help establish the required geometry between the probe and the orbiter for radio communications during the probe descent on 14 January. It also shows that the probe and Cassini are well within the predicted trajectory accuracy. So how could we check the spin rate was correct? When the Huygens probe was being designed more than 10 years ago, it was required that the probe had to be magnetically 'clean' when switched off, meaning that any residual permanent magnetic fields must not interfere with the sensitive Cassini magnetometers. Later, when the probe was built, it was found that there was still a weak magnetic field produced, but within acceptable limits for Cassini's magnetometer sensors. However, because magnetic fields have a 'direction' as well as a strength, and this weak field was slightly off-center, it effectively gave the probe a 'left' and a 'right' side (it behaves like a small magnet with a north and south pole). With the implication being that if you can detect this magnetic field, then you can also detect how it is rotating.
Following an initial suggestion by Jean-Pierre Lebreton, the Huygens Project Scientist, scientists on the Cassini Dual Technique Magnetometer (MAG) team, from Imperial College, London, and Braunschweig, confirmed that their instrument should be able to detect this small rotating magnetic field and plans were put in place to measure this during the probe release period. Magnetometers are direct-sensing instruments that detect and measure both the strength and direction of magnetic fields in the vicinity of the instrument. The Cassini MAG is measuring these fields while Cassini is in orbit around Saturn as well as during the close Titan encounters. But, just after separation on 25 December, the MAG scientists detected fluctuations in the magnetic field around Cassini that could only have come from Huygens rotating and moving away. Professor Michele Dougherty, Principal Investigator for MAG, said, "What was observed by MAG just after the probe separation on 25 December 2004, were weak but clear fluctuations in both magnetic sensors which reside on the 11-meter magnetometer boom. These fluctuations were a clear indication of the Huygens probe moving away from the Cassini orbiter. This signature confirmed the spin rate of the probe at 7.5 revolutions per minute, the ideal rate which was predicted, and that Huygens is well on its way to Titan." Former MAG Principal Investigator David Southwood, who is now the Director of Science at ESA, said, "Detecting the spin was immensely reassuring - not only did it show Huygens was rotating correctly, but also because the spin is directly related to the departure velocity, that Huygens was headed off at the right speed. It was really great to do it with an instrument I knew so well."
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