| Aerobraking, part 2 |
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Slowing it Down
Atmospheric drag - the friction the spacecraft experiences as it passes
through the top layer of the atmosphere - slows down the spacecraft.
Each pass brings the spacecraft to a lower altitude. Repeated "drag
passes" as they are called are conducted to shape the spacecraft's
trajectory from its initial elliptical, egg-shaped orbit into the desired circular orbit.
The design of each drag pass is carefully worked out by navigators,
spacecraft engineers and scientists who measure the results of the
preceding pass, read measurements and estimate the height and density
of the atmosphere, predict the atmosphere's effect on the spacecraft's
structure, and determine the best entry and exit points to achieve the
orbital geometry required for the mission.
Aerobraking is extremely challenging but worth it, say mission engineers,
because it eliminates the need for the heavy load of extra propellant that
would otherwise be needed to place the spacecraft in its desired orbit.
Aerobraking Saves Cost and Mass
A large, heavy spacecraft requires a large, expensive launch vehicle. NASA
has successfully driven down costs of space exploration missions by using
smaller spacecraft for launch on smaller, less costly rockets
than those used for most interplanetary missions in the past. Research
and development dedicated to new technology is delivering ever-smaller
miniaturized instrumentation and electronics. As a result, most
interplanetary spacecraft today are less than half as large as spacecraft
designed 10 or more years ago, and these can be launched on relatively small rockets.
But no matter how small the spacecraft, if it is destined to orbit another
planet, it must have the means to slow down once it gets there in order to
be captured into orbit. (Aerocapture, a close cousin of aerobraking, is an
as-yet-untested technique that would use the friction of a planetary
atmosphere to actually capture a spacecraft into orbit. This would
eliminate the need for most of the large amount of fuel now needed for
delivering a spacecraft into the desired orbit around Mars.) Once a
spacecraft is captured, it still needs to reach the particular orbital geometry
required for the mission. So far, two means exist to move the spacecraft
into the desired orbit: chemical rockets or aerobraking.
Even for a small-sized spacecraft, a massive amount of propellant is
required for an orbit insertion. Almost half of Odyssey's total mass is
simply rocket fuel that will be expended in the approximately 20-minute
Mars orbit insertion engine firing. Without aerobraking, even more
propellant would have to have been added to the spacecraft to bring
Odyssey into its final orbit. The additional mass would have pushed the
spacecraft weight beyond the capability of the low-cost launch vehicle and
required a larger, more expensive rocket.
Odyssey's Aerobraking
Odyssey's aerobraking occurs in three primary phases that engineers
call 'walk-in', 'the main phase' and 'walk-out'. The walk-in phase occurs
during the first four to eight orbits following Mars arrival. That phase will
be used as a calibration period so that engineers can understand how the
spacecraft behaves in and out of aerobraking. It will help determine the
adequacy of the Odyssey team's aerobraking plans and ensure their
assumptions about Mars' atmosphere.
Martian dust storms, which can dramatically change the height and
density of the atmosphere, are a particular concern during aerobraking.
The mission's first Mars image, to be taken by the
thermal emission imaging system
in the early phase of aerobraking, will test its capability to look at the
atmosphere to detect dust storms. Also on the lookout for dust storms is
Odyssey's sibling spacecraft, Mars Global Surveyor,
already in orbit at Mars. If for some reason Global Surveyor is unavailable
for that purpose, Odyssey's thermal emission imaging system, which is
partly an infrared camera, will be used for atmospheric monitoring of Mars.
The main aerobraking phase begins once the point of the spacecraft's
closest approach to the planet has been lowered to within about 100
kilometers (about 60 miles) above the Martian surface. (That point is known
as the orbit's "periapsis") Approximately 380 "drag
passes", the term to describe the spacecraft's flight through the
atmosphere, will be accomplished in 78 days. Each pass will reduce the
altitude of the spacecraft and "trim" its orbit into a more
circular flight path. With each pass too, the spacecraft's point of closest
approach to Mars will move northward eventually drifting over Mars' north
pole and then back down the "other side" of the planet.
The Odyssey team will periodically use the onboard jets to make
adjustments before some passes through the atmosphere. Such adjustments
might need to be made if the spacecraft is found to be flying too high or
too low in the atmosphere.
The aerobraking drag passes will be flown under the direction of
commands stored in the central onboard computer. Each pass commences
with a warm-up of the small thrusters used to make any last minute
adjustments. The radio transmitter is turned off to conserve power during
the drag pass; the power savings are important because Odyssey will
temporarily be without use of its solar panels. The solar panels double as
an aerobraking "drag chute", and must be secured to the
body of the spacecraft to face into the martian atmosphere. Battery power
supplies electricity during aerobraking.
Odyssey's gyro-like reaction wheels now spin to adjust the spacecraft's
orientation in space, pointing the solar panels down to brush the top of
Mars' atmosphere.
The walk-out phase occurs during the last few days of aerobraking.
At that time, Odyssey's orbit will still be egg-shaped. The lowest point
(periapsis) will be near an altitude of 120 kilometers (75 miles) and is
most distant point (apoapsis) will be near the 400-kilometer (250-mile)
altitude planned for the mission. Onboard thrusters will be fired to raise
the periapsis to achieve the final 400-kilometer (250-mile) circular science orbit.
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