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The BepiColombo spacecraft is on its way to Mercury

lpetrich

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Earlier this evening, US Pacific Time, the BepiColombo spacecraft was successfully launched to Mercury atop an Ariane 5 rocket from ESA"s spaceport in Kourou, French Guiana, South America (BepiColombo Spacecraft on 7-Year Trek to Mercury for Europe and Japan,  BepiColombo).

BepiColombo will be the third spacecraft to visit that planet, after Mariner 10 (3 flybys in 1974-75) and MESSENGER (orbited 2011-15).

It will take seven years to make the trip, flying by the Earth once, Venus twice, and Mercury six times, and also using its ion engines for much of the trip. These flybys and the ion-engine thrust are all necessary to slow down the spacecraft so that it will be able to go into orbit around Mercury without needing much velocity change or delta-V.

The next scheduled event is flying by the Earth about 1 1/2 years from now in early 2020. Late that year, the spacecraft will fly by Venus, and 1 1/3 years later, in mid 2021, it will fly by Venus again. Two months later, it will fly by Mercury, after five more flybys, it will go into orbit around that planet late in 2025. It will then observe the planet and its environs for the next 2 or 3 years.

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As the spacecraft travels, its operators will use tracking data to help improve two tests of general relativity, "post-Newtonian" parameters gamma and beta. The first one is (amount of space curvature) / (amount of time curvature), and the second one is the amount of nonlinearity in the time curvature. The Newtonian limit is the lowest order of that curvature. The first one is involved in the delay and deflection of light and radio waves near massive objects, and both of them are involved in extra orbit precession over what one would predict from the planets pulling on each other.

That extra precession is most easily observable for Mercury, and it was discovered in the mid nineteenth century by Urbain Leverrier. He attributed it to an intra-Mercurian planet or planets, but despite several claimed observations, it was not possible to assemble a coherent orbit from them, and astronomers grew skeptical of the existence of such planets. Over the last century, upper limits on the sizes of such putative planets have been forced far down, recently to some 20 kilometers, the size of a small asteroid.

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The spacecraft itself has three parts: the Mercury Transfer Module, the Mercury Planetary Orbiter, and Mio (Mercury Magnetospheric Orbiter). The MTM will propel and support the MPO and Mio for the trip, and it will detach shortly before MPO goes into orbit with Mio. After entering orbit, MPO will release Mio and then propel itself into its final orbit closer to the planet.

Mio (MMO) is Japan's contribution to this mission. It will have some instruments for measuring the magnetic field and the interplanetary medium at the spacecraft.

MPO contains instruments for exploring the planet's surface and atmosphere -- a very thin atmosphere. It will have cameras, spectrometers for visible light, IR, UV, X-rays, gamma rays, neutrons, and charged particles, and also a laser altimeter -- all contributed by several nations.

Omitted for budgetary reasons was a proposed lander and rover.

But if this mission is a success, it will return a lot of nice data on Mercury.
 
A lander/rover would be very limited (geographically speaking) in where it could go, wouldn't it? I would assume one would have to stay within a few hundred or so km of the poles?

Also, 7 years seems like a long time to get to Venus. Is that intentional to accommodate the other space/time curvature experiments, or just due to the delta V requirements and weight budget?
 
A lander/rover would be very limited (geographically speaking) in where it could go, wouldn't it? I would assume one would have to stay within a few hundred or so km of the poles?
Likely, so it would not get too hot in the daytime.
Also, 7 years seems like a long time to get to Venus. Is that intentional to accommodate the other space/time curvature experiments, or just due to the delta V requirements and weight budget?
That's Mercury, not Venus. It's because of the necessary delta-V for getting there.

If one does a simple transfer orbit, like what one does for Venus or Mars, one will be moving at 9.61 km/s relative to Mercury when one arrives there. That is almost the Earth's escape velocity. To get down to Mercury's escape velocity of 4.25 km/s, one will need a delta-V of 6.26 km/s at closest approach to Mercury. It's not linear because of something called the Oberth effect, an outcome of conservation of energy. That's almost as much delta-V as one needs to go into orbit around our planet, so one would need a big rocket.
 
What a view! Mercury probe snaps stunning photos of our planet during Earth flyby. | Space - on April 10

The article has a picture and an animation of some pictures of our planet, and also a picture of the spacecraft by an Earth-based observer. It looked like a star in it - it wasn't resolved by that observer's telescope.

The spececraft's next journey milestones:
  • Venus flybys: 2020 Oct 15, 2021 Aug 11
  • Mercury flybys: 2021 Oct 2, 2022 Jun 23, 2023 Jun 20, 2024 Sep 5, 2024 Dec 2, 2025 Jan 9
  • Mercury orbit insertion: 2020 Dec 5
  • MPO in final science orbit: 2026 Mar 14
  • End of nominal mission: 2027 May 1
  • End of extended mission: 2028 May 1

The spacecraft has three parts, parts that will travel together and separate at Mercury:
  • Mercury Transfer Module (MTM) for propulsion, built by ESA
  • Mercury Planetary Orbiter (MPO) built by ESA
  • Mercury Magnetospheric Orbiter (MMO) or Mio built by JAXA
(quoting Wikipedia)

Each part will go into a separate orbit. Both orbits will be polar orbits, with altitudes
  • MPO: 480 km * 1500 km (300 mi * 930 mi)
  • MMO: 590 km * 11,640 km (370 mi * 7,230 mi)
 
ESA - BepiColombo
Bepi (@ESA_Bepi) / Twitter
BepiColombo (@BepiColombo) / Twitter

Lots of pictures from the October 2 flyby of Mercury, the first of six. Also some pictures from the one Earth and the two Venus flybys. In the Earth pictures, one can see East Africa, Arabia, and the Indian Subcontinent. It's grayscale, and the land areas are a little brighter than the oceans, with the clouds being much brighter. But in the Venus pictures, Venus looks almost featureless.
 
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