冥卫一星上曾存在地下海洋

If the icy surface of Pluto¹'s giant moon Charon is cracked, analysis of the fractures could reveal if its interior was warm, perhaps warm enough to have maintained a subterranean²（地下的，秘密的） ocean of liquid water, according to a new NASA-funded study. Pluto is an extremely distant world, orbiting the sun more than 29 times farther than Earth. With a surface temperature estimated to be about 380 degrees below zero Fahrenheit³ (around minus 229 degrees Celsius), the environment at Pluto is far too cold to allow liquid water on its surface. Pluto's moons are in the same frigid⁴ environment.

 

Pluto's remoteness and small size make it difficult to observe, but in July of 2015, NASA's New Horizons spacecraft will be the first to visit Pluto and Charon, and will provide the most detailed⁵ observations to date.

 

"Our model predicts different fracture patterns on the surface of Charon depending on the thickness of its surface ice, the structure of the moon's interior and how easily it deforms⁶, and how its orbit evolved," said Alyssa Rhoden of NASA's Goddard Space Flight Center in Greenbelt, Maryland. "By comparing the actual New Horizons observations of Charon to the various predictions, we can see what fits best and discover if Charon could have had a subsurface ocean in its past, driven by high eccentricity⁷（古怪，离心率）." Rhoden is lead author of a paper on this research now available online in the journal Icarus.

 

Some moons around the gas giant planets in the outer solar system have cracked surfaces with evidence for ocean interiors -- Jupiter's moon Europa and Saturn's moon Enceladus are two examples.

 

As Europa and Enceladus move in their orbits, a gravitational tug-of-war between their respective parent planets and neighboring moons keeps their orbits from becoming circular. Instead, these moons have eccentric (slightly oval-shaped) orbits, which raise daily tides that flex⁸ the interior and stress the surface. It is thought that tidal heating has extended the lifetimes of subsurface oceans on Europa and Enceladus by keeping their interiors warm.

 

In Charon's case, this study finds that a past high eccentricity could have generated large tides, causing friction⁹ and surface fractures. The moon is unusually massive compared to its planet, about one-eighth of Pluto's mass, a solar system record. It is thought to have formed much closer to Pluto, after a giant impact ejected material off the planet's surface. The material went into orbit around Pluto and coalesced¹⁰ under its own gravity to form Charon and several smaller moons.

 

Initially¹¹, there would have been strong tides on both worlds as gravity between Pluto and Charon caused their surfaces to bulge¹²（膨胀） toward each other, generating friction in their interiors. This friction would have also caused the tides to slightly lag behind their orbital positions. The lag would act like a brake on Pluto, causing its rotation¹³ to slow while transferring that rotational¹⁴ energy to Charon, making it speed up and move farther away from Pluto.

 

"Depending on exactly how Charon's orbit evolved, particularly if it went through a high-eccentricity phase, there may have been enough heat from tidal deformation¹⁵ to maintain liquid water beneath the surface of Charon for some time," said Rhoden. "Using plausible¹⁶ interior structure models that include an ocean, we found it wouldn't have taken much eccentricity (less than 0.01) to generate surface fractures like we are seeing on Europa."

 

"Since it's so easy to get fractures, if we get to Charon and there are none, it puts a very strong constraint¹⁷ on how high the eccentricity could have been and how warm the interior ever could have been," adds Rhoden. "This research gives us a head start on the New Horizons arrival -- what should we look for and what can we learn from it. We're going to Pluto and Pluto is fascinating, but Charon is also going to be fascinating."

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