Study shows Saturn moon Enceladus' ocean may have hydrothermal activity

CU-Boulder-led study shows Saturn moon's ocean may have hydrothermal activity
A team led by CU-Boulder has shown that Saturn's icy moon Enceladus is spewing tiny silica grains, an indication hydrothermal activity is occurring in its ice-covered ocean. Such extreme environments are known to be suitable for life on Earth. Credit: NASA/JPL

A new study by a team of Cassini mission scientists led by the University of Colorado Boulder have found that microscopic grains of rock detected near Saturn imply hydrothermal activity is taking place within the moon Enceladus.

The grains are the first clear indication of an icy moon having hydrothermal activity, in which seawater infiltrates and reacts with a rocky crust, emerging as a heated, mineral-laden solution. The finding adds to the tantalizing possibility that Enceladus, one of at least 60 Saturn moons or moonlets and which displays remarkable geologic activity including geysers, could contain environments suitable for living organisms.

The results are being published March 12 in the journal Nature.

The surprising new result follows an extensive, four-year analysis of data from the spacecraft, computer simulations and laboratory experiments. From their examination, the researchers determined the tiny grains most likely form when hot water containing dissolved minerals from the moon's rocky interior travels upward, coming into contact with cooler water.

Temperatures required for the interactions that produce the tiny rock grains would be at least 194 degrees Fahrenheit (90 degrees Celsius).

"It's very exciting that we can use these tiny grains of rock, spewed into space by geysers, to tell us about conditions on—and beneath—the ocean floor of an icy moon," said Research Associate Sean Hsu at CU-Boulder's Laboratory for Atmospheric and Space Physics, lead author on the paper.

Study shows Saturn moon Enceladus's ocean may have hydrothermal activity
This artist's impression of the interior of Saturn's moon Enceladus shows that interactions between hot-water and rock occur at the floor of the subsurface ocean. This activity eventually brings hydrothermal reaction products up through the 40-50 km ice crust and into the giant plume of gas and ice that erupts into space from the moon's south polar region. Credit: NASA/JPL-Caltech

Cassini's Cosmic Dust Analyzer (CDA) instrument has repeatedly detected miniscule rock particles, rich in the element silicon, near Saturn since 2004. By process of elimination, the CDA team concluded these particles must be grains of silica, which is found on Earth in sand and the mineral quartz. The consistent size of the grains observed by Cassini—the largest of which were 6 to 9 nanometers—was the clue that told the researchers a specific process likely was responsible.

On Earth, the most common way to form silica grains of this size is hydrothermal activity involving a specific range of conditions: namely, when slightly alkaline water with modest salinity that is super-saturated with silica undergoes a big drop in temperature.

"We methodically searched for alternate explanations for the nano-silca grains, but every new result pointed to a single, most likely origin," said Frank Postberg, a Cassini CDA team scientist at Heidelberg University in Germany, and a co-author on the paper.

Hsu and Postberg worked closely with colleagues at the University of Tokyo who performed the detailed laboratory experiments that validated the hydrothermal activity hypothesis. The Japanese team, led by Yasuhito Sekine, verified the conditions under which silica grains form at the same size Cassini detected. The researchers think these conditions may exist at the seafloor on Enceladus, where hot water from the interior meets the relatively cold water at the ocean bottom.

The Nature paper co-authors also included CU-Boulder Professor Mihaly Horanyi and Assistant Professor Sascha Kempf of LASP. Both also are faculty members in CU-Boulder's physics department and co-investigators of the Cassini CDA.

According to Kempf, the puzzle of the Enceladus plumes—first identified not long after the Cassini spacecraft reached the realm of Saturn in 2004—has been solved, at least to some extent. "Ten years ago it was a big mystery why the nano-grains were made of silica rather than water ice," Kempf said. "Now we know the observations were correct. We know where the silica particles are coming from, and why we are seeing them. We learned something very unexpected, which is why I really like this study."

This NASA image from April 4, 2014 shows a diagram that illustrates the possible interior of Saturn's moon Enceladus based on a
This NASA image from April 4, 2014 shows a diagram that illustrates the possible interior of Saturn's moon Enceladus based on a gravity investigation by NASA's Cassini spacecraft and NASA's Deep Space Network

The extremely small size of the silica particles also suggests that they travel upward relatively quickly from their hydrothermal origin to the near-surface sources of the moon's now famous geysers. From seafloor to outer space, a distance of about 30 miles (50 kilometers), the spend a few months to a few years in transit, otherwise they would grow to much larger sizes.

Cassini first revealed active geology on Enceladus in 2005 with evidence of an icy spray issuing from the moon's south polar region and higher-than-expected temperatures in the icy surface there. The mission soon revealed a towering plume of water ice and vapor, salts and organic materials that issues from relatively warm fractures on the wrinkled surface. Gravity measurements published in 2014 strongly suggest the presence of a 6-mile-deep (10-kilometer) ocean beneath an ice shell about 19 to 25 miles (30 to 40 kilometers) thick.

The authors point out that Cassini's gravity measurements suggest Enceladus' rocky core is quite porous, which would allow water from the ocean to percolate into the interior. This would provide a huge surface area where rock and water could interact.

"It's possible much of this interesting chemistry occurs deep inside the moon's core," Hsu said.


Explore further

Strongest evidence yet indicates Enceladus hiding saltwater ocean

More information: Nature, dx.doi.org/10.1038/nature14262
Journal information: Nature

Citation: Study shows Saturn moon Enceladus' ocean may have hydrothermal activity (2015, March 11) retrieved 22 July 2019 from https://phys.org/news/2015-03-saturn-moon-enceladus-ocean-hydrothermal.html
This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no part may be reproduced without the written permission. The content is provided for information purposes only.
3718 shares

Feedback to editors

User comments

Mar 12, 2015
The nursery of life!

Please sign in to add a comment. Registration is free, and takes less than a minute. Read more