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First visit to Pluto could rewrite the solar system’s story

Rivers of neon, geysers of nitrogen, an oddly giant moon: the New Horizons probe promises revealing spectacles – and insights into deep solar system history
First visit to Pluto could rewrite the solar system's story

Pluto: welcome to the planet that was (Image: Marie Bergeron)

FOUR and a half light-hours from Earth, a small planet is about to get a small visitor. On 14 July, NASA’s craft will skim within just 13,000 kilometres of Pluto, entering a hitherto-unexplored zone of the solar system.

When this probe was launched in January 2006, its destination was still the solar system’s ninth planet. Pluto was controversially demoted to a dwarf planet later that year, but its allure is undiminished. Above its surface, frosted with exotic ices, is a strange atmosphere that seeps constantly into space, and a complex system of moons, including the giant Charon. Pluto will be a dazzling destination in itself, and this first visit could also give us clues to how our own planet formed, and to the ancient upheavals that shaped the solar system. With the blobs of Pluto and Charon already swelling in New Horizons’s sights, these are exciting times at the solar system’s new frontier.

Until recently, this frontier seemed a lonely one, with Pluto its sole denizen. Then, in the 1990s, astronomers began finding further icy bodies in this remote region of the sort that might make comets. More and more followed, forming a swarm of debris stretching far out beyond the orbit of Neptune – an area now known as the Kuiper belt.

The Kuiper belt’s icy shrapnel is thought to be left over from the birth of the eight major planets, remnants long ago hurled out into their present dark domain. Many are dwarf planets on Pluto’s scale – a diverse bunch, with different colours and shapes and satellite systems. “The Kuiper belt is littered with small planets – and Pluto is the archetype,” says of the Southwest Research Institute in Boulder, Colorado, who is principal investigator on the New Horizons mission.

None of this was known back in the 1980s when Stern began to push for a Pluto mission: he was mainly looking for a place to explore. “This was a chance for a new generation of scientists to mount a mission to a new place. There were no other new places to go.”

First visit to Pluto could rewrite the solar system's story

The New Horizons probe almost didn’t get off the ground (Image: NASA/JHUAPL/SwRI)

Pluto’s realm – dark, cold and far from home – is tough territory. Solar panels are no use at this distance, so New Horizons runs on heat from the radioactive decay of a lump of plutonium. Under such weak sunlight an unheated probe would cool to below -200 °C, so New Horizons is cosseted in a multilayer blanket that traps waste heat from its instruments and electrical systems, keeping its interior at about room temperature.

Radio signals take 9 hours for a round trip to Earth, so the spacecraft must be highly autonomous. And with a 12-watt transmitter on board, the signal is so weak that it can carry only about a kilobit of information per second across 5 billion kilometres. Precious images and other discoveries from the fly-by will take 16 months to download.

“9 hours for a signal to travel from Earth to Pluto and back”

Just getting the spacecraft off the ground was a challenge. Several times a mission was proposed and studied, then ditched. “If the mission had been a cat it would have been dead long ago, because cats only get nine lives,” says Stern. “It was not just political intrigues, but the road to build and launch on time, with plutonium shortages and almost impossible schedules. There were so many problems.”

Progress since blast-off has by contrast been serene. In 2007 New Horizons flew by Jupiter to gain a gravitational kick, and tested its cameras and other instruments. They revealed lightning at Jupiter’s poles, the Tvashtar volcano erupting on the moon Io and signs of a recent impact in Jupiter’s rings – as well as a surprising lack of small moons.

Since then, the trip has mostly been spent in hibernation mode. “We’ve been in cruise for so long you get used to the pace: ‘What’s new this month? The spacecraft is OK’,” says , a planetary scientist at Washington University in St Louis, Missouri. “Now after all this time, something’s really happening.”

That “something” might yet be calamitous. When they were building the spacecraft, scientists expected the Pluto system to be relatively hazard-free. Then Pluto’s smaller moons were discovered: Nix and Hydra in 2005, Kerberos in 2011 and Styx in 2012. When another object from the Kuiper belt hits one of them, it could kick up a cloud of shrapnel that would escape the moon’s weak gravity. At the speed New Horizons is travelling, even a small pebble or ice shard could be catastrophic.

“248 years for Pluto to orbit the sun”

The latest simulations suggest that the chance of a serious collision is slim, but right now the team are analysing images to look for new moons or rings that might increase the hazard. They have contingency plans to change course and avoid any danger zones, though that would mean a slightly more restricted view of Pluto.

While New Horizons analyses dust and ionised gas around Pluto, most eyes will be on the dwarf planet itself (see diagram). Already the probe has seen signs of a polar cap and other surface features, and as it closes in two imagers will scan Pluto’s surface in more and more detail. LORRI, equipped with a small telescope, will capture black-and-white images with a resolution of about 70 metres at closest approach; another, called Ralph, will furnish the colour pictures. Ralph can also analyse infrared light, and should reveal the detailed chemical make-up of Pluto’s landscape.

First visit to Pluto could rewrite the solar system's story

From the way Pluto’s brightness changes as it spins, we know that methane, nitrogen and carbon monoxide ices form changing patterns on its surface, but what that landscape looks like remains a mystery. Probably the closest model is Neptune’s giant moon Triton, thought to be an ex-Pluto long ago captured from an independent life in the Kuiper belt. “Triton has very unusual landscapes,” says McKinnon. In 1989 NASA’s outer solar system probe Voyager 2 sent back pictures of Triton’s “cantaloupe terrain“, which looks like nothing in the solar system so much as the skin of a cantaloupe melon. Along with fresh lava flows, Triton’s relatively new terrain is a sign of geological activity driven from within. “This is a mystery,” says Stern. “We don’t know how to power small worlds like this. Pluto will be a second data point.”

“4.8 billion km Current distance of New Horizons from Earth”

McKinnon will be looking for signs that may betray a buried ocean of water. “We don’t have an ocean detector device, we can’t X-ray Pluto, so we’ll be looking for clues from its shape and landscape,” he says. Those include fracture patterns that might indicate the presence of a subsurface reservoir. “The holy grail would be evidence of past eruptions, or active vents,” says McKinnon.

Perhaps, like Triton, Pluto has active geysers of nitrogen gas, powered by faint sunlight. It certainly has a tenuous nitrogen atmosphere with pressures a few millionths that of Earth’s. Without a supply of fresh gas the atmosphere would not last long, because under Pluto’s weak gravity it is leaking into space, even enveloping Charon. Nitrogen on the surface must be going direct from the frozen to the gaseous state; winds are then thought to blow from the day to the night side, where the gas refreezes.

“-228° Celsius Pluto’s surface temperature”

New Horizons will find out more about the composition of Pluto’s atmosphere using an instrument called Alice to analyse the spectrum of starlight filtering through it. The spacecraft will also send radio signals through the atmosphere and back to Earth, where mission scientists can work out temperature and pressure profiles from the signal distortion.

Rivers of neon

Wispy though it is, this atmosphere allows some outlandish possibilities. Liquid neon might be stable, suggests hydrologist Jeff Kargel of the University of Arizona in Tucson. Then neon could play the part of water on Earth and methane on Saturn’s moon Titan, and run in rivers across Pluto’s surface.

McKinnon is doubtful. “I’m not expecting rivers of liquid neon, but you never know,” he says. “We are going to see something we haven’t seen before, and that will delight us.” His own suggestion is that liquid nitrogen could flow in places under Pluto’s ice, and that a large impact could inject enough heat to melt lakes of nitrogen on the surface, or even .

So there seems little chance that Pluto will turn out to be a dull, dead world, a disappointing space rock marked only by impact craters. “But I hope to see some craters,” says McKinnon. For one thing, Pluto’s craters could be a key to understanding how planets came into being.

Our traditional picture of planet formation starts with small grains that collide and build into boulders, then larger and larger objects. If this is right, the Kuiper belt should hold leftover planetary building blocks of all sizes. But that idea is undermined by Jupiter’s moon Europa. Europa’s surface is only a few tens of millions of years old, having been renewed perhaps by a process akin to plate tectonics. Being so new, it only shows recent comet impacts. There are relatively few small craters, meaning a lack of small comets hitting Europa. “We would expect many times more kilometre-sized things,” says , a colleague of Stern’s at the Southwest Research Institute who specialises in the dynamics of planetary systems. “Maybe those things go ‘poof’ and disappear when they come into the inner solar system and are heated by the sun. Or maybe they never got created.”

Counting craters of different sizes on Pluto gives an idea of how many iceballs are hitting it and how big they are. These scars should show us whether those kilometre-scale building blocks really are missing from the Kuiper belt – and whether we need a new theory of planet formation. One recent idea is called : little pebbles a few centimetres across gather into large groups which then suddenly collapse under gravity. “You go directly to objects 10 to 100 kilometres in size,” says Levison.

Even if Pluto’s nitrogen craters have evaporated away, there should be a good cratering record on its outsize moon, Charon. Charon is so large that it and Pluto arguably make up a binary system (see “Charon’s secrets“). Its probable origin in a giant collision could shed light on the violent events that shaped the young solar system once the planets had formed.

Roughly 4 billion years ago, it’s thought, the young giant planets moved outwards through a dense disc of debris girdling the sun, in the process hurling comets in all directions. Some came our way, and huge impacts created the moon’s “seas” and scourged Earth in a trauma known as the Late Heavy Bombardment. Most models rely on Neptune and Uranus migrating out like this, but it’s not clear when and how fast, or how Jupiter moved around, or just what the original debris disc was like.

The collision that formed Charon probably happened before all this, so working out exactly how it happened could tell us a little about that disc and how it became today’s Kuiper belt. Researchers had expected the Kuiper belt to be a settled, flattish disc of objects in nice circular orbits. Instead, it is a mess. “It looks like someone took the solar system, picked it up and shook it really hard,” says Levison. Again, the giant planets were probably responsible, but no existing models can match the real tangle of orbits. “Pluto’s formation and evolution is going to give us hints to what happened in the entire outer planetary system,” says Levison.

First visit to Pluto could rewrite the solar system's story

There’s only one chance to get things right, so just at the moment, the mission team is rather busy. “We are navigating by taking images and analysing them and computing rocket burn simulations,” says Stern. “We are looking for hazards, testing programs that will operate the spacecraft during the encounter, and preparing more than 150 software tools for data analysis. I’m not worried about anything we’ve thought of; I worry about what we haven’t thought of.”

A first scan for hazards has come up clear. And as Pluto gradually comes into sharper focus, new features already suggest a complex surface. Come 14 July, things will happen fast. Just a few minutes after closest approach, New Horizons will turn to scan Charon, then back to Pluto to map its southern polar regions, hidden on the approach. That side of Pluto is currently turned away from the sun, so the only light will be a faint glow reflected from Charon.

Then, after this all-too-brief encounter it’s onwards and outwards, probably towards PT1 (“potential target 1”), a Kuiper belt object 1.5 billion kilometres further from the sun, and just a few tens of kilometres across. After that, the spacecraft will join the earlier Pioneer and Voyager probes as part of Earth’s interstellar flotilla, reporting on the state of the solar wind until its plutonium power fades away.

But first and last things first. The first world of the Kuiper belt, or the last of the nine planets if you prefer, is coming into view.

Read more:Fly by Pluto with the New Horizons probe

LeaderOur exploration of the solar system is just getting started

The hunt for Planet X

First visit to Pluto could rewrite the solar system's story
A strangely mobile blob (arrows) identified in 1930 hinted at a new planet (Image: Lowell Observatory Archives)

All the clues pointed to something big out there. In the late 19th century, astronomers suspected that anomalies in the orbits of Uranus and Neptune were caused by the gravity of a large, unseen planet. They spent decades, on and off, searching for “Planet X”, to no avail. Then, in 1930, Clyde Tombaugh at the Lowell Observatory in Flagstaff, Arizona, spotted something. He was checking photographic plates of an area in the constellation Gemini, using a device called a blink comparator to flick between plates taken on separate nights. On 18 February he found a small dot that had moved between two dates in January (see pictures).

Being so far away, stars are effectively stationary as seen from Earth, so it had to be something within our solar system. Its motion turned out to be too slow for an asteroid whirling around the inner solar system. Instead, the object had to be out beyond the orbit of Neptune, and it looked planet-sized. The dot was named Pluto after the Roman god of the underworld.

But Pluto is not the hoped-for Planet X: it is far too small to have the observed effect on Uranus and Neptune. Only in 1992 did new data, including a measurement of Neptune’s mass by Voyager 2, allow those apparent orbital anomalies to vanish. Rumours still persist, but Planet X is probably now fading into myth – having helped us find Pluto.

Topics: Pluto / Solar system