Lecture 15 - Mercury and Venus

Chapter 8: Mercury

8.1: Orbital Properties

  • Mercury's orbit is highly elliptical, with an eccentricity of e=0.206e = 0.206.
  • The average Sun-Mercury distance is 0.39 AU.
  • Perihelion distance (closest to the Sun): 0.32 AU.
  • Aphelion distance (farthest from the Sun): 0.48 AU.
  • Elongation is the angle between Mercury and the Sun as viewed from Earth.
    • Perihelion elongation: 18°
    • Aphelion elongation: 28°
  • Mercury is never far from the Sun in the sky when viewed from Earth.
  • It is only visible just before sunrise or just after sunset.
  • The maximum elongation of Mercury is 28°.
  • It is visible for no more than about 2 hours.
  • Mercury shines by reflected sunlight, like the Moon.
  • Phases of Mercury are best seen at maximum elongation.
  • The semimajor axis of Mercury's orbit is a=0.39a = 0.39 AU.
  • Kepler's Third Law allows calculation of Mercury's orbital period.
  • Orbital Period Formula: P2 (in Earth years)=a3 (in AU)P^2 \text{ (in Earth years)} = a^3 \text{ (in AU)}
  • Orbital Period: P=0.24P = 0.24 Earth years = 88 Earth days

8.2: Physical Properties

  • Mercury's size is similar to the Moon, but its density is similar to Earth.
  • Radius: 2440 km
  • Mass: 3.3×10233.3 \times 10^{23} kg
  • Density: 5400 kg/m3
  • Escape Speed: 4.2 km/s
  • Mercury's size is comparable to some moons in the solar system, such as Ganymede, Titan, Callisto, and Io.

8.4: Rotation Rate

  • Initially, Mercury was believed to be tidally locked to the Sun, with a synchronous orbit and a rotation period of 88 Earth days.
  • Radar measurements in 1965 determined Mercury's rotation period to be 59 Earth days, exactly two-thirds of a Mercury year.
  • Mercury's orbital and rotational motions combine to create a solar day that is 2 Mercury years long.
  • Mercury spins 3 times for every 2 orbits around the Sun, resulting in a 3:2 resonance.
  • The 3:2 resonance occurs because Mercury's orbit is highly eccentric.
  • Mercury's rotation speed (spin on its axis) is constant, but its orbital speed varies between aphelion and perihelion.
  • Spin and orbital rates are equal at perihelion but not at aphelion.
  • The Sun's tidal forces have created a tidal bulge on Mercury.
  • If spin and orbital rates are out of sync, the Sun will pull the bulge to re-establish resonance.
  • The same face of Mercury points toward the Sun every other time it is at perihelion, resulting in a 3:2 resonance.

Mercury's Atmosphere

  • Mercury has no significant atmosphere.
  • Being close to the Sun, any gas molecules near its surface have fast thermal motion.
  • The escape speed is only 4.2 km/s, so any gas molecules would have easily escaped.
  • Without an atmosphere to moderate the surface temperature, and with one Mercury day equaling 59 Earth days, the daily temperature variation is extreme.
  • Tday=700T_{\text{day}} = 700 K (above the boiling point of water)
  • Tnight=100T_{\text{night}} = 100 K (below the freezing point of water)
  • Mercury is heavily cratered like the Moon due to the lack of an atmosphere providing protection from meteoroid impacts.
  • Most information about Mercury has come from the Mariner 10 and Messenger spacecraft.
  • Mariner 10:
    • Launched in 1973 (stopped returning data in 1975)
    • Passed by Mercury every six months
    • Mapped 45% of the surface with 4000 photographs
  • Messenger:
    • Orbited Mercury from 2011-2015
    • Created detailed surface maps
    • Studied composition
    • Found water ice in craters

8.3: Surface Features

  • Mercury is less heavily cratered than the Moon.
  • Intercrater plains were formed by volcanic activity (3.9 to 3.7 billion years ago), covering older craters.
  • There is no evidence of plate tectonics.
  • Due to higher gravity than on the Moon:
    • Crater walls are not as high.
    • Ejecta material landed closer to the crater.
    • Many large craters on Mercury have dark material around them, but the origin is not fully understood.

8.6: The Surface of Mercury

  • Scarps (cliffs):
    • Not fault lines, as there are no tectonic plates
    • Hundreds of km long and up to 3 km high
    • Younger than most craters
    • Occurred after a bombardment that liquefied the surface
    • As the surface cooled, it cracked
  • Hollows:
    • Lighter-colored, irregularly shaped depressions on a crater's rim and floor
    • Formed when the Sun's heat vaporized loose material in the crater
    • Not seen anywhere else in the solar system
  • Caloris Basin:
    • Very large impact feature
    • 1400 km diameter
    • Ringed by mountain ranges that reach more than 3 km high
    • On the opposite side of the planet from