Lecture 15 - Mercury and Venus
Chapter 8: Mercury
8.1: Orbital Properties
- Mercury's orbit is highly elliptical, with an eccentricity of e=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=0.39 AU.
- Kepler's Third Law allows calculation of Mercury's orbital period.
- Orbital Period Formula: P2 (in Earth years)=a3 (in AU)
- Orbital Period: P=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: 3.3×1023 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=700 K (above the boiling point of water)
- Tnight=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