The oceans are one big electrolyte solution. They have a lot of salt and other minerals. Life on Earth is not the same without the oceans' electrolyte content. It may not beexistent.

Different processes on Earth release electrolytes into the ocean.

Is it possible to get life-enabling vitamins on water worlds?

Water worlds are planets with water. Some of the exoplanets we have discovered are expected to be water worlds. electrolytes play a similar role in habitability that they do on Earth's oceans.

The interiors of super-Earths and mini-Neptunes are under more pressure than the Earth's. Deep planetary ice mantles can be formed between the rocky core and the ocean. There are ice barriers. The dense ice could prevent essential mineral electrolytes from moving from the core to the ocean, where they would be available for life.

Habitability of ocean worlds could be limited by these high-pressure ice barriers. electrolytes can flow through the ice on water worlds according to a new study. There is one more reason to be positive about life in these worlds.

The study shows the stability of high- temperature salty ice. The author is a researcher at the European Synchrotron Radiation Facility.

The paper says that lytes play an important role in the internal structure and dynamics of water-rich satellites. The presence of a large high-pressure ice mantle is thought to affect the exchange and transport of electrolytes.

This is an artist’s impression of TRAPPIST-1e, a potential water world. Planets like this may have submerged mantles of high-pressure ice that act as a barrier to nutrient flow. Image Credit: By NASA/JPL-Caltech – Cropped from PIA22093: TRAPPIST-1 Planet Lineup – Updated Feb. 2018, Public Domain, https://commons.wikimedia.org/w/index.php?curid=76364487

Earth's ice is similar to the ice in the mantles. There are ice types on larger planets. Ice I is the regular Earth ice. Researchers created Ice VII after dropping water to a powerful shock wave.

In ocean worlds that are mini-Neptunes, the deeper layers of the ocean are likely frozen into ice. The structure of Ice VII is different than that of Ice I. According to the simulations, the ice can hold a lot of vitamins and minerals.

It's important that Ice VII has a characteristic. VII ice has 2.5% of NaCl in its structure by weight. The ice has a melting point. The currents from the inside of the planet can propel the NaCl into the ocean. That causes the ice to cool and sink again. Salt from the planet's rocky interior is recycled up through the ice mantle into the ocean.

This figure from the study shows how NaCl can be released from an exoplanet's silicate mantle and flow upward due to convection. Image Credit: Hernandez et al. 2022.
This figure from the study shows how NaCl can be released from an exoplanet’s silicate mantle and flow upward due to convection. Image Credit: Hernandez et al. 2022.

This could be happening in our solar system. Some of the icy moons are stained with hydrated salt minerals. There are HP ice mantles at different depths that form barriers between the rocky core and the oceans on many moons. The minerals were transported through ice. The moons aren't massive enough to form Ice VII, but they are massive enough to form mantles of high pressure ice.

This diagram shows what the interior of Ganymede, the largest moon in the Solar System, might look like. Layers of the ocean with different salinities might be sandwiched between layers of ice with different structures. Image Credit: NASA/JPL–Caltech
This diagram shows what the interior of Ganymede, the largest moon in the Solar System, might look like. Layers of the ocean with different salinities might be sandwiched between layers of ice with different structures. Image Credit: NASA/JPL–Caltech

It could be a game-changer if salt can be transported from a planet's rocky interior to the ocean. There is more evidence that the ocean world could support life.

We see more water worlds as we find more planets. TRAPPIST-1e and TRAPPIST-1f are strong candidates, though scientists aren't sure. Water worlds are also possible with the addition of the two new ones.

The Kepler 62 system is about 990 light-years from Earth and hosts two potential water worlds, 62e and 62f. Image Credit: NASA Ames/JPL-Caltech - http://www.nasa.gov/mission_pages/kepler/news/kepler-62-kepler-69.html, Public Domain, https://commons.wikimedia.org/w/index.php?curid=25666606
The Kepler 62 system is about 990 light-years from Earth and hosts two potential water worlds, 62e and 62f. Image Credit: NASA Ames/JPL-Caltech – http://www.nasa.gov/mission_pages/kepler/news/kepler-62-kepler-69.html, Public Domain, https://commons.wikimedia.org/w/index.php?curid=25666606

He is a researcher at the University of Washington, where he studies planetary sciences. A commentary was written on this study. Ocean worlds are likely widespread according to his article. There are no ocean worlds in our solar system. Our planet is remarkably dry, even though it is two-thirds ocean.

Earth might be two-thirds covered in water, but it's nowhere near being an ocean planet. Image Credit: USGS.
Earth might be two-thirds covered in water, but it’s nowhere near being an ocean planet. Image Credit: USGS.

New results have boosted the habitability potential of all of the ocean worlds. The most convincing argument yet in resolving the dilemma of large planetary hydroosphere habitability is offered by the study.

Several geologic processes can release minerals from a planet's rocky core into an icy mantle. According to this new study, the dense ice in the mantle allows nutrients to be transported to the surface ocean on ocean planets. Image Credit: Baptiste Journaux
Several geologic processes can release minerals from a planet’s rocky core into an icy mantle. According to this new study, the dense ice in the mantle allows nutrients to be transported to the surface ocean on ocean planets. Image Credit: Baptiste Journaux

There is no way to see ocean exoplanets in their full glory. The JWST might change that. It may be possible to detect fingerprints from ocean planet's atmosphere There is more assistance on the way.

Some of the Solar System's icy/ ocean moons are being developed by NASA and the European Space Agency. In 2031, the Jovian system will be reached by the Jupiter Icy Moons Explorer. The solar system's largest moon will be entered in 20 34. It will eventually approach the surface of the moon.

Jupiter is expected to be reached by 2030. Even though it will be in the air, it will be studying another ocean moon.

High-pressure water ice mantles can be formed by giants. It is far from certain if there will be a mission to the largest moon in the solar system.

Ganymede is massive enough to form one or more layers of high-pressure ice. If this new study is correct, then critical electrolytes may be able to cycle between the moon's rocky core and its oceans, something that boosts any chances of habitability. Image Credit: By National Oceanic and Atmospheric Administration
Ganymede is massive enough to form one or more layers of high-pressure ice. If this new study is correct, critical electrolytes may be able to cycle between the moon’s rocky core and its oceans, which boosts any chances of habitability. Image Credit: By National Oceanic and Atmospheric Administration

Some of the conclusions will be tested by the missions to these moons. Habitability on water worlds is dependent on the ability to transport electrolytes through high-pressure ice layers. Life requires more than just two words. We don't know if other important molecule can pass through these barriers.

The upcoming missions will show us a lot about our Solar System's icy ocean moons. The findings will also apply to other solar systems. These missions will allow us to better understand the inner-workings of the hydroospheres of icy moons and will be key to understanding the largest oceans in our universe in water-rich exoplanets.

Some of the other factors involved in ocean world habitability are discussed by the authors.

There are many factors that need to be considered for an ocean planet. They demonstrated that it is possible with their simulations.

We will have to wait and see if their simulations are correct.

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