Psyche (spacecraft)

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Psyche
Mission type Reconnaissance
Operator NASA
Mission duration 2 years (proposed)
Start of mission
Launch date 2020 (proposed)
16 Psyche asteroid orbiter
Orbital insertion 2026 (proposed)[1]

Psyche is a proposed orbiter mission concept by NASA to explore the origin of planetary cores by studying the metallic asteroid 16 Psyche. This asteroid is the exposed iron core of a protoplanet, likely the remnant of a violent collision with another object that stripped off the outer crust.

16 Psyche is the heaviest known M-type asteroid, and heaviest known Themistian asteroid. Radar observations of the asteroid from Earth indicate an iron–nickel composition.[2]

Overview

A 3D model of 16 Psyche based on lightcurve data

Psyche was selected on 30 September 2015 as one of five semifinalists for the Mission #13 of the Discovery Program.[3] The winner will be chosen around September 2016,[4] and must be ready to launch by the end of 2021.[5][6] The Psyche spacecraft would use solar electric propulsion,[7] and the notional payload would be an imager, a magnetometer, and a gamma-ray spectrometer.[7] [8]


The mission would launch in 2020 and arrive in 2026 for a year of science.[1] Data shows 16 Psyche asteroid to have a diameter of about 252 km (157 mi).[9] Linda Elkins-Tanton of Arizona State University in Tempe, Arizona is the Principal Investigator. NASA's Jet Propulsion Laboratory would manage the project.

Objectives

The Widmanstätten pattern that can be found inside iron–nickel meteorites. Some iron–nickel meteorites found on Earth may have come from Psyche.[2]

Differentiation was a fundamental process in shaping many asteroids and all terrestrial planets, and direct exploration of a core could greatly enhance understanding of this process. The Psyche mission would characterize 16 Psyche's geology, shape, elemental composition, magnetic field, and mass distribution. It is expected that this mission will increase the understanding of planetary formation and interiors. The science questions this mission will address are: [10]

  1. Is asteroid 16 Psyche the stripped core of a differentiated planetesimal, or was it formed as an iron-rich body? What were the building blocks of planets? Did planetesimals that formed close to the Sun have very different bulk compositions?
  2. If 16 Psyche was stripped of its mantle, when and how did that occur?
  3. If 16 Psyche was once molten, did it solidify from the inside out, or the outside in?
  4. Did 16 Psyche produce a magnetic dynamo as it cooled?
  5. What are the major alloy elements that coexist in the iron metal of the core?
  6. What are the key characteristics of the geologic surface and global topography? Does 16 Psyche look radically different from known stony and icy bodies?
  7. How do craters on a metal body differ from those in rock or ice?

See also

References

  1. ↑ 1.0 1.1 Lua error in package.lua at line 80: module 'strict' not found.
  2. ↑ 2.0 2.1 33th Largest Asteroid, 16 Psyche
  3. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  4. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  5. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  6. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  7. ↑ 7.0 7.1 Lua error in package.lua at line 80: module 'strict' not found.
  8. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  9. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  10. ↑ Lua error in package.lua at line 80: module 'strict' not found.

External links

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