Mercury, the tiniest and least-explored planet within the internal photo voltaic system, is hiding mysteries far bigger than itself — and at last, scientists will quickly be getting not one however two spacecraft designed to decode the unusual world.
That is due to the BepiColombo mission, a joint challenge of the European Area Company (ESA) and Japan Aerospace Exploration Company (JAXA) that launched in October 2018. After a harrowing journey by means of the internal photo voltaic system, the mission is tackling an important maneuver on Thursday (Sept. 3): separating its science gear from the transport that carried all of it that method. By April 2027, scientists hope the mission’s two instrument-heavy probes will probably be gathering a slew of observations that would assist remedy puzzles about Mercury — and possibly even the photo voltaic system we name house.
“I feel having the ability to see new knowledge come out about Mercury goes to be so unbelievable,” Rachel Klima, a planetary geologist on the Johns Hopkins College Utilized Physics Laboratory, advised Area.com. The planet, she says, is “simply so bizarre and delightful and attention-grabbing.”
An enigmatic planet
For now, Mercury holds the doubtful honor of being the least-explored planet within the internal photo voltaic system, visited by solely two missions to this point. NASA’s Mariner 10 spacecraft made a trio of zippy flybys in 1974 and 1975, giving scientists their first glimpses of the planet’s cracked and cratered surface, as well as confirming the world has both a very tenuous atmosphere and a magnetic field.
“It really gave us our first close-up view of Mercury,” Sean Solomon, a planetary scientist at Columbia University, told Space.com. “But it left a lot of pages blank.”
And for decades, that was it. Scientists didn’t return to Mercury until 2011, when NASA’s MESSENGER spacecraft, with Solomon as its principal investigator, arrived at the tiny world. (Mercury has a radius of 1,516 miles, or 2,440 kilometers, meaning its width is just over a third of Earth’s.) The spacecraft was packed with tools tailored to the job, such as spectrometers tuned to gamma-rays, X-rays and neutrons, and instruments to sniff out the atmosphere and measure the magnetic field, and it was there to stay. Four years of observations with MESSENGER showed scientists Mercury’s complete surface for the first time, and by late in its mission, the spacecraft was passing just 15.5 miles (24.9 km) above the planet’s surface.
But even MESSENGER wasn’t sophisticated enough to crack Mercury’s puzzles or unveil the strange planet’s beginnings. “I think the jury’s still out on exactly how Mercury got assembled,” Solomon said.
MESSENGER opened up some smaller mysteries, too. It discovered bright, steep-sided pits that scientists dubbed “hollows.” It found a suite of elements — that planetary scientists call “volatiles” for their tendency to slip free of rock — somehow more prevalent in Mercury’s surface than Earth’s. It calculated that the center of the planet’s magnetic field is wildly offset from the planet’s core. Plus, MESSENGER’s tricky orbit also meant the spacecraft never saw the southern half of the planet as sharply as the northern half, leaving one side shadowed in doubt.
The arrival of BepiColombo
It’s these mysteries that the ambitious BepiColombo mission hopes to tackle. By April, if all goes well, the mission will consist of two separate spacecraft gathering independent but coordinated data about Mercury.
Europe’s Mercury Planetary Orbiter, or MPO, will focus on the planet proper. It’s packed with 11 science instruments that will map the terrain, minerals in the crust, and the gravity field, investigate the hollows and volcanic deposits, and observe how the barrage of charged particles from the sun affects this innermost planet.
Japan’s Mercury Magnetospheric Orbiter, or Mio, meanwhile, will focus on the planet’s surroundings — its magnetosphere and wispy atmosphere, as well as the dust cluttering up its neighborhood.
Both spacecraft also carry instruments to measure the planet’s magnetic field, offering simultaneous observations of different parts of the field to scientists who typically make do with data gathered from just one location at a time.
In fact, some of these instruments have been able to gather observations during BepiColombo’s long trek to Mercury and its six quick flybys of the planet so far. But because of how the spacecraft were configured for the journey, most of the instruments have not — and will not — get to work until after MPO and Mio have separated. That is expected to happen in December.
The mission’s science, then, has begun only in dribbles, while the bulk of its promise still lies ahead. “There is a growing literature of new results that have come from the BepiColombo flybys, but I expect that will explode once they go into orbit,” Solomon said.
He’s especially excited to see the spacecraft’s sharp views of the southern hemisphere, and particularly find hidden deposits of water ice across the area. These deposits would exist in deep craters that never feel the sun’s heat. In examining this region of the planet, scientists will be able to reduce the northerly bias of MESSENGER’s data and better see Mercury’s complete picture.
Meanwhile, Klima is most eagerly awaiting MPO’s work to map elements and minerals in the planet’s surface. This work eluded MESSENGER, which used a technique that relied on these rocks being rich in iron and similar materials — but as it turned out, those elements were absent, leaving scientists stymied. MPO carries different technology that will be able to read rocks on the world even without iron, which Klima said could help reveal how Mercury — and our whole solar system, as a matter of fact — formed.
Klima says she hopes BepiColombo can get people excited about Mercury, the overlooked terrestrial planet of the solar system: “It certainly doesn’t get the love and attention that Mars and Venus and everywhere else gets.”