Deep beneath the icy surface of Saturn’s moon Enceladus, something’s happening that causes particles of icy silica to spew out to space.
They eventually end up in Saturn’s E ring. Planetary scientists knew that this was happening, but didn’t have a good explanation for why or how. Now, they do.
A new study done by a team at the University of California Los Angeles offers some answers. Their work shows that tidal heating in Enceladus’ rocky core creates currents (or flows) that transport the silica. Then, it’s probably released by deep-sea hydrothermal vents over the course of just a few months.
“Our research shows that these flows are strong enough to pick up materials from the seafloor and bring them to the ice shell that separates the ocean from the vacuum of space,” said Ashley Schoenfeld, a doctoral student at UCLA. “The tiger-stripe fractures that cut through the ice shell into this subsurface ocean can act as direct conduits for captured materials to be flung into space. Enceladus is giving us free samples of what’s hidden deep below.”
Why Enceladus Spews its Secrets
Data from the missions that visited the Saturn system keep revealing surprises about the Saturnian moons. We now know that Enceladus is an ocean world, for example. That’s because it has a large volume of liquid water mostly locked away beneath the icy surface. The surface itself is extremely reflective and has cracks that allow fountains of icy particles to escape into space. Those so-called “tiger stripes” provide an exit point for the icy silica.
Those particles start out on the sea floor deep beneath the surface. The tidal forces that squeeze Enceladus under the grip of Saturn’s strong gravity deform this little moon. That creates friction in the surface as well as the rocky core underneath the ocean. That sets up currents in the watery ocean.
A rendering of the sediment capture model developed in the UCLA-led study, showing buoyancy effects on silica grains produced at hydrothermal vents along the sea floor and how this eventually leads to their escape through cracks in the outer ice shell of Enceladus. Courtesy: Ashley Schoenfeld/UCLA; NASA/JPL.
Hydrothermal Activity Plays a Role Inside Enceladus
Although the Voyager mission first revealed the strange surface of Enceladus, it wasn’t until Cassini made its long-term studies that planetary scientists found the plumes jetting out from the tiger stripes. The spacecraft measured large amounts of hydrogen gas in those plumes. That’s pretty strong evidence of hydrothermal activity on the ocean floor.
Hydrothermal vents deep in Earth’s oceans. Could similar types of vents power the transport of silica and other materials out from Enceladus? Credit: NOAA
Hydrothermal heating on Earth happens near volcanically active places beneath the sea, particularly in mid-ocean ridges. Those are where tectonic plates are spreading apart. That action allows volcanic material to spew up from beneath and superheat the water. On Enceladus, the friction caused by tidal heating creates hotspots that feed the currents carrying silica particles to space.
The UCLA team led by Schoenfeld created a model to simulate that process. It also allowed them to estimate a timeframe for it. Their model also explains why the currents are transporting other materials to the surface in addition to the silica. “Our model provides further support to the idea that convective turbulence in the ocean efficiently transports vital nutrients from the seafloor to ice shell,” said second author Emily Hawkins, a UCLA alumna who is now an assistant professor of physics at Loyola Marymount University.
Of course, the presence of heat and water raises the question of whether Enceladus is hospitable to life. On Earth, hydrothermal vents support an amazing variety of life forms. It remains for future missions to Enceladus to pin that down. They could study places inside that moon to see if it could support life. Those efforts would require landers to gather more information both on the ice and deep in the subsurface ocean.
Source: Universetoday.com
