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   » » Wiki: Protoplanet
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A protoplanet or planetary embryo is a -sized astronomical body originated within a protoplanetary disk that has undergone to produce a differentiated interior, and has the potential to further evolve into a planetary-mass object. Protoplanets are thought to form out of kilometer-sized that gravitationally perturb each other's orbits and collide, gradually coalescing into larger bodies through a process known as "runaway growth".

(2023). 9783662650929, . .
Once accumulated enough , protoplanets will begin to assume a spherical shape due to hydrostatic equilibrium and become , those of which that subsequently succeed in dominating their own orbit will become proper.

An alternative formation pathway of protoplanets is a process called disk fragmentation. Formation by this process, also called gravitational (disk) instability, is favoured for giant planets on wide orbits.


The planetesimal hypothesis
A is an object formed from dust, rock, and other materials, measuring from meters to hundreds of kilometers in size. According to the Chamberlin–Moulton planetesimal hypothesis and the theories of , a protoplanetary disk of materials such as gas and dust would orbit a star early in the formation of a planetary system. The action of on such materials form larger and larger chunks until some reach the size of planetesimals.

It is thought that the collisions of planetesimals created a few hundred larger planetary embryos. Over the course of hundreds of millions of years, they collided with one another. The exact sequence whereby planetary embryos collided to assemble the planets is not known, but it is thought that initial collisions would have replaced the first "generation" of embryos with a second generation consisting of fewer but larger embryos. These in their turn would have collided to create a third generation of fewer but even larger embryos. Eventually, only a handful of embryos were left, which collided to complete the assembly of the proper.

(2025). 9780521837354, Cambridge University Press.

Early protoplanets had more elements, the quantity of which has been reduced over time due to radioactive decay. Heating due to radioactivity, impact, and gravitational pressure melted parts of protoplanets as they grew toward being planets. In melted zones their heavier sank to the center, whereas lighter elements rose to the surface. Such a process is known as planetary differentiation. The composition of some show that differentiation took place in some .


Evidence in the Solar System - surviving remnant protoplanets
In the case of the , it is thought that the collisions of planetesimals created a few hundred planetary embryos. Such embryos were similar to Ceres and with masses of about 1022 to 1023 kg and were a few thousand kilometers in diameter.

According to the giant impact hypothesis, the formed from a colossal impact of a hypothetical protoplanet called Theia with Earth, early in the Solar System's history.

In the inner Solar System, the three protoplanets to survive more-or-less intact are the Ceres, Pallas, and Vesta. Psyche is likely the survivor of a violent hit-and-run with another object that stripped off the outer, rocky layers of a protoplanet. The asteroid Metis may also have a similar origin history to that of Psyche. The asteroid Lutetia also has characteristics that resemble a protoplanet. have also been referred to as protoplanets. Because have been found on Earth, it is deemed likely that there once were other metal-cored protoplanets in the that since have been disrupted and that are the source of these meteorites.


Extrasolar protoplanets - observed protoplanets
The first directly imaged exoplanet candidates were confirmed in 2005. Several of them are very young, , GQ Lupi b, 2M1207b and show signs of accretion. However, all these candidates either lack in confirmation of a planetary mass or in confirmation that they formed within the protoplanetary disk of the host object.

In January 2012 astronomers made the first direct observation of a candidate protoplanet forming in a disk of gas and dust around a distant star, LkCa 15. Subsequent observations, however, refuted the existence of this candidate.

In February 2013 astronomers made the first direct observation of a candidate protoplanet, that is still a candidate, forming in a disk of gas and dust around a distant star, HD 100546. Subsequent observations suggest that several protoplanets may be present in the gas disk.

Another protoplanet, AB Aur b, may be in the earliest observed stage of formation for a gas giant. It is located in the gas disk of the star . AB Aur b is among the largest exoplanets identified, and has a distant orbit, three times as far as Neptune is from the Earth's sun. Observations of AB Aur b may challenge conventional thinking about how planets are formed. It was viewed by the and the Hubble Space Telescope.

Rings, gaps, spirals, dust concentrations and shadows in protoplanetary disks could be caused by protoplanets. These structures are not completely understood and are therefore not seen as a proof for the presence of a protoplanet. One new emerging way to study the effect of protoplanets on the disk are molecular line observations of protoplanetary disks in the form of gas velocity maps. HD 97048 b is the first protoplanet detected by disk in the form of a kink in the gas velocity map.

+List of confirmed protoplanets (described as "protoplanets" in literature) !Star !Exoplanet !Mass
() !Period
(yr) !Separation
(AU) !Distance to Earth
() !Year of Discovery !Detection technique
PDS 70PDS 70 b 11920 ± 21122018Direct Imaging
PDS 70 c 227341122019Direct Imaging
HD 97048HD 97048 b2.5 ± 0.59561301842019Disk Kinematics
HD 169142HD 169142 b3 ± 216737.2± 1.51142019/2023Direct imaging


Unconfirmed protoplanets
The confident detection of protoplanets is difficult. Protoplanets usually exist in gas-rich protoplanetary disks. Over-densities within these disks can mimic protoplanets. A number of unconfirmed protoplanet candidates are known and some detections were later questioned.
+List of unconfirmed/disputed/refuted protoplanets !Star/host !Exoplanet !Mass
() !Period
(yr) !Separation
(AU) !Distance to Earth
() !Year of Discovery !Status !Detection technique
DH Tauri b8-50 3301352005unconfirmed planetary mass and formation in diskDirect imaging
GQ Lupi b1-36 1031522005unconfirmed planetary mass and formation in diskDirect imaging
2M12072M1207b5-6 49.8652005unconfirmed formation in diskDirect imaging
LkCa 15LkCa 15 b 12.7 2012refuted in 2019Direct imaging
LkCa 15 c 18.6 2015Direct imaging
LkCa 15 d 24.7 2015Direct imaging
HD 100546HD 100546 b4–1324953 ± 21082015disputed in 2017Direct imaging
Gomez's HamburgerGoHam b 350 ± 502502015unconfirmed candidateDirect imaging
AB Aur b9–20 94 ± 491562022disputed in 2023 and 2024Direct imaging
2–3 110 2022unconfirmed candidateDisk Kinematics
HD 163296multiple? 2022unconfirmed candidatesDisk Kinematics
Elias 2-24 2–5 52 2023unconfirmed candidateDirect imaging + Disk Kinematics


See also


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