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                     Magellan Fact Sheet

* Mission Summary *

 The Magellan spacecraft, named after the sixteenth-century
 Portuguese explorer whose expedition first circumnavigated the
 Earth, was launched May 4, 1989, and arrived at Venus on
 August 10, 1990.  Magellan's solid rocket motor placed it into
 a near-polar elliptical orbit around the planet.  During the
 first 8-month mapping cycle around Venus, Magellan collected
 radar images of 84 percent of the planet's surface, with
 resolution 10 times better than that of the earlier Soviet
 Venera 15 and 16 missions.  Altimetry and radiometry data also
 measured the surface topography and electrical
 characteristics.  During subsequent cycles the map will be
 completed, filling gaps in coverage from the first cycle and
 imaging the south polar region for the first time.  Precision
 radio tracking of the spacecraft will measure Venus'
 gravitational field to show the planet's internal mass
 distribution and the forces which have created the surface
 features.  Magellan's data will permit the first global
 geological understanding of Venus, the planet most like Earth
 in our solar system.

* Venus *

 Distance from Sun:            1.1 x 108 km
 Orbit Period:                 225 Earth days
 Radius:                       6051 km
 Rotational Period (sidereal): 243 Earth days 
 Average Density:              5.2 g/cm3
 Surface Gravity:              .907 times that of Earth
                               (8.87 m/s2)
 Surface Temperature:          850 F (730 K)
 Surface Atmospheric Pressure: 90 times that of Earth
                               (90 q 2 bar)
 Atmospheric Composition:      Carbon dioxide (96%); nitrogen
                               (3+%); trace amounts of sulfur
                               dioxide, water vapor, carbon
                               monoxide, argon, helium, neon,
                               hydrogen chloride, hydrogen
                               fluoride

* Major Mission Characteristics *

 Interplanetary Cruise:        May 4, 1989, to August 10, 1990
 First Mapping Cycle:          September 15, 1990 to May 15,
                               1991
 Orbit Period:                 3.25 hours
 Orbit Inclination:            86 degrees
 Radar Mapping Per Orbit:      37.2 minutes
 Planetary Coverage:           84%
 Extended Mission Plan:        May 16, 1991 to May 15, 1993
 Cycle 2:                      Image the south pole region and
                               gaps from Cycle 1
 Cycle 3:                      Fill remaining gaps and collect
                               stereo imagery
 Cycle 4:                      Measure Venus' gravitational
                               field

* Mission Objectives *

 Obtain near-global radar images of Venus' surface, with
 resolution equivalent to optical imaging of 1 km per line pair
 Obtain a near-global topographic map with 50km spatial and
 100m vertical resolution
 Obtain near-global gravity field data with 700km resolution
 and 2-3 milligals accuracy
 Develop an understanding of the geological structure of the
 planet, including its density distribution and dynamics

* Magellan Team *

 NASA/Solar System Exploration Division
  1. Elizabeth E. Beyer, Program Manager
  1. Joseph M. Boyce, Program Scientist
  1. David J. Okerson, Program Engineer
 JPL
  1. James F. Scott, Project Manager
  1. R. Stephen Saunders, Project Scientist
  1. Douglas G. Griffith, Mission Directory
 Principal Investigators
  1. Radar: Gordon Pettengill (MIT)
  1. Gravity: William Sjogren (JPL)
                               Georges Balmino (France)
 System Contractors
  1. Spacecraft: Martin Marietta/Denver
                               F. McKinney, Manager
  1. Radar: Hughes Aircraft
                               B. Dagarin, Manager

* Key Spacecraft Characteristics *

 Single radar instrument operates simultaneously (by
 interleaving) in Synthetic Aperture Radar (SAR), altimeter,
 and radiometer modes
 High Gain Antenna (3.7m diameter) is used as both the radar
 and telecommunications antenna
 X-band downlink data rate of 268.8 or 115 kbps
 Coherent X- and S-band radio subsystem used for gravity field
 measurement by precision tracking of the spacecraft's orbit
 Spacecraft on-orbit dry mass of 1035 kg
 Monopropellant hydrazine thruster system (0.9 to 445N thrust)
 Powered by solar panels with rechargeable batteries
 Three orthogonal electrically powered reaction wheels used for
 spacecraft pointing control

* Key Radar Characteristics *

 Synthetic Aperture Radar (SAR)
  1. Frequency 2.385 GHz
  1. Peak Power 325 W
  1. Pulse Length 26.5 msec
  1. PRF 4400-5800 Hz
  1. Swath Width 25 km (variable)
  1. Data Acquisition Rate 806 kbps
  1. Downlink Quantization 2 bits
 Operates in SAR, altimeter, and radiometer modes
  1. SAR Resolution 150m range/150m azimuth
  1. Altimeter Resolution 30m
  1. Radiometer Accuracy 2 C
 Operating parameters controlled by ground command

* Key Scientific Results *

 A preliminary assessment of the Magellan high-resolution
 global images is providing evidence to understand the role of
 impacts, volcanism, and tectonism in the formation of Venusian
 surface structures.
 The surface of Venus is mostly covered by volcanic materials. 
 Volcanic surface features, such as vast lava plains, fields of
 small lava domes, and large shield volcanoes are common.
 There are few impact craters on Venus, suggesting that the
 surface is, in general, geologically young - less than 800
 million years old.
 The presence of lava channels over 6,000 kilometers long
 suggests river-like flows of extremely low-viscosity lava that
 probably erupted at a high rate.
 Large pancake-shaped volcanic domes suggest the presence of a
 type of lava produced by extensive evolution of crustal rocks.
 The typical signs of terrestrial plate tectonics - continental
 drift and basin floor spreading - are not in evidence on
 Venus.  The planet's tectonics is dominated by a system of
 global rift zones and numerous broad, low domical structures
 called coronae, produced by the upwelling and subsidence of
 magma from the mantle.
 Although Venus has a dense atmosphere, the surface reveals no
 evidence of substantial wind erosion, and only evidence of
 limited wind transport of dust and sand.  This contrasts with
 Mars, where there is a thin atmosphere, but substantial
 evidence of wind erosion and transport of dust and sand.

* For More Information on Data *

 Photographic images, digital data (CD ROMs) and display
 software, and videotapes showing computer-generated flights
 over Venus are available to researchers, educators, and the
 public through the National Space Science Data Center, Goddard
 Space Flight Center, Mail Code 933.4, Greenbelt, MD 20771,
 (301) 286-6695, Fax: (301) 286-4952.
 Detailed catalog information is available to researchers funded by 
 NASA's Solar System Exploration Division through the Planetary Data 
 System, Geosciences Node, Earth and Planetary Remote Sensing 
 Laboratory, Washington University St. Louis, MO 63130-4899, 
 (314) 935-5493, Fax: (314) 935-7361.
 Photographic imagery, CD-ROMs, and videotapes are available
 for browsing at NASA's 15 Regional Planetary Image Facilities. 
 For additional information, call Mary Ann Harger at the Lunar
 and Planetary Institute at (713) 486-2136 or -2172, Fax: (713)
 486-2153.
 Teachers can obtain information about Magellan, including
 copies of the videotapes, through NASA's Teacher Resource
 Centers.  For more information, call the Jet Propulsion
 Laboratory's Teacher Resource Center at (818) 354-6916, Fax:
 (818) 354-8080.
/home/gen.uk/domains/wiki.gen.uk/public_html/data/pages/archive/science/magellan.txt · Last modified: 2001/11/04 06:14 by 127.0.0.1

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