Accretion theory suggests gas giants might start out as steamy worlds

November 8, 2017 by Bob Yirka, Phys.org report
Schematic diagram showing several evolutionary stages of a protoplanet accreting ice-rich pebbles. (1) Planet without an atmosphere. (2) Planet with an atmosphere and a solid ice/rock surface. The outer atmosphere is radiative. The inner atmosphere is convective with ice grains precipitating towards the surface. (3) Planet with a rocky core and an ocean. The outer atmosphere is radiative, and the inner atmosphere is convective with ice and water precipitation. (4) Planet with a rock core and no ocean. The outer atmosphere is radiative, and the inner atmosphere is convective. Precipitation occurs at mid altitudes, but the deep atmosphere is too hot for water to condense or undersaturated. Credit: arXiv:1710.03134 [astro-ph.EP]

(Phys.org)—John Chambers, a planetary scientist with the Department of Terrestrial Magnetism at Carnegie Institution has suggested a new theory regarding the formation of gas giant planets. In his paper uploaded to the preprint server arXiv, soon to be published in the Astrophysical Journal, he describes his theory and its possible implications.

The origins of such as Jupiter are believed to be similar to those of rocky planets—via accretion of material circling their star. It is believed they become gas giants due to their distance from their star and the limited impact of stellar winds. In this new effort, Chambers offers a new, more detailed theoretical description of the process.

Chambers suggests that accretion from rocks as small as pebbles and ice could have led to the formation of a protoplanet with slowly increasing atmospheric pressure—that, he says, would have caused the ice to sublimate, filling the atmosphere with water particles—he describes it as a steamy world. As time passes, heat from the star would cause the protoplanet to grow warmer and gain more mass, and the atmospheric pressure to rise, which in turn would allow the atmosphere to hold even more water. At some point, he notes, the pressure would become so great that the water would become a supercritical fluid—a mix of hydrogen and helium. That, he suggests, would lead to a runaway situation in which the protoplanet begins pulling in gasses from the disk around its star—continually growing until it depletes available gas, reaching its ultimate size.

This new theory by Chambers notably differs from other theories that suggest that planets tend to form from large, kilometer-sized chunks of space debris. But it does conform to another theory that suggests that gas giants must form relatively quickly because thin dramatically as the star ages.

Chambers notes that even if his theory is correct, he is still not sure if it would apply to Jupiter, though there is some recent evidence suggesting that the gas giant has a core that is more diffuse than has been generally thought.

Explore further: Could Trappist-1's seven earth-like planets have gas giant siblings?

More information: Steamworlds: atmospheric structure and critical mass of planets accreting icy pebbles, arXiv:1710.03134 [astro-ph.EP] arxiv.org/abs/1710.03134

Abstract
In the core accretion model, gas-giant planets first form a solid core, which then accretes gas from a protoplanetary disk when the core exceeds a critical mass. Here, we model the atmosphere of a core that grows by accreting ice-rich pebbles. The ice fraction of pebbles evaporates in warm regions of the atmosphere, saturating it with water vapor. Excess water precipitates to lower altitudes. Beneath an outer radiative region, the atmosphere is convective, following a moist adiabat in saturated regions due to water condensation and precipitation. Atmospheric mass, density and temperature increase with core mass. For nominal model parameters, planets with core masses (ice + rock) between 0.08 and 0.16 Earth masses have surface temperatures between 273 K and 647 K and form an ocean. In more massive planets, water exists as a super-critical convecting fluid mixed with gas from the disk. Typically, the core mass reaches a maximum (the critical mass) as a function of the total mass when the core is 2-5 Earth masses. The critical mass depends in a complicated way on pebble size, mass flux, and dust opacity due to the occasional appearance of multiple core-mass maxima. The core mass for an atmosphere of 50 percent hydrogen and helium may be a more robust indicator of the onset of gas accretion. This mass is typically 1-3 Earth masses for pebbles that are 50 percent ice by mass, increasing with opacity and pebble flux, and decreasing with pebble ice/rock ratio.

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5 comments

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barakn
not rated yet Nov 08, 2017
At some point, he notes, the pressure would become so great that the water would become a supercritical fluid—a mix of hydrogen and helium.
The oxygen magically transforms into helium?
jonesdave
5 / 5 (2) Nov 08, 2017
At some point, he notes, the pressure would become so great that the water would become a supercritical fluid—a mix of hydrogen and helium.
The oxygen magically transforms into helium?


No, the H & He are already there. As they say in the paper:

At core masses slightly higher than in Figure 3, an ocean ceases to exist. Instead the entire water budget exists as either water vapor or a super-critical fluid. We assume that the water becomes intimately mixed with the hydrogen and helium throughout the resulting atmosphere.
Nik_2213
5 / 5 (1) Nov 08, 2017
sorry, #b, the article's editor dropped a few vital words from the 'abstract', munging it...
Caliban
not rated yet Nov 08, 2017
Also, the idea of a core is somewhat muzzy in the first place, since it assumes that the "rocky" portion of the protoplanetary disc extends all the way out to the outermost edge of the solar system in question.

The core may accrete before, during, or after the formation of the gaseous planet itself. To say that a gaseous planet has to have a rocky core to accrete around is not necessarily an accurate portrayal, since the disc itself consists of a "slurry" of varying density and proportion of gas and dust. Local density sufficient to create gravitational attraction greater than the average velocity in that region of the disc would be enough to begin planetary accretion, whether that local density was primarily gaseous or not. More of a sliding scale sort of problem.
cantdrive85
1.8 / 5 (5) Nov 08, 2017
Accretion theory suggests gas giants might start out as steamy worlds

The title of the article needs a slight adjustment...
'Accretion theory is a steamy pile of BS'

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