Some Sun-like stars are “Earth-eaters.” During their development, they ingest large amounts of the rocky material from which terrestrial” planets like Earth, Mars, and Venus are made.
Trey Mack from Vanderbilt University in Nashville, Tennessee, has developed a model that estimates the effect that such a diet has on a star’s chemical composition and has used it to analyze a pair of twin stars that both have their own planets.
“Trey has shown that we can actually model the chemical signature of a star in detail, element by element, and determine how that signature is changed by the ingestion of Earth-like planets,” said Keivan Stassun from Vanderbilt. “After obtaining a high-resolution spectrum for a given star, we can actually detect that signature in detail, element by element.”
This ability will add substantially to astronomers’ understanding of the process of planet formation as well as assisting in the ongoing search for Earth-like exoplanets, according to the astronomers.
First, some background: Stars consist of more than 98 percent hydrogen and helium. All the other elements make up less than 2 percent of their mass. Astronomers have arbitrarily defined all the elements heavier than hydrogen and helium as metals and have coined the term “metallicity” to refer to the ratio of the relative abundance of iron to hydrogen in a star’s chemical makeup.
Since the mid-1990s, when astronomers developed the capability to detect extrasolar planets in large numbers, there have been several studies that attempt to link star metallicity with planet formation. In one such study, researchers at Los Alamos National Laboratory argued that stars with high metallicities are more likely to develop planetary systems than those with low metallicities. Another study concluded that hot Jupiter-sized planets are found predominantly circling stars with high metallicities while smaller planets are found circling stars with a wide range of metal content.
Building on the work of co-author Simon Schuler of the University of Tampa, who expanded the examination of stars’ chemical composition beyond their iron content, Mack looked at the abundance of 15 specific elements relative to that of the Sun. He was particularly interested in elements like aluminum, silicon, calcium, and iron that have melting points higher than 1200° Fahrenheit (600° Celsius) because these are the refractory materials that serve as building blocks for Earth-like planets.
Mack, Schuler, and Stassun decided to apply this technique to the planet-hosting binary pair designated HD 20781 and HD 20782. Both stars should have condensed out of the same cloud of dust and gas, so both should have started with the same chemical compositions. This particular binary pair is the first one discovered where both stars have planets of their own.
Both of the stars in the binary pair are G-class dwarf stars similar to the Sun. One star is orbited closely by two Neptune-sized planets. The other possesses a single Jupiter-sized planet that follows a highly eccentric orbit. The difference in their planetary systems make the two stars ideal for studying the connection between exoplanets and the chemical composition of their stellar hosts.
When they analyzed the spectrum of the two stars, the astronomers found that the relative abundance of the refractory elements was significantly higher than that of the Sun. They also found that the higher the melting temperature of a particular element, the higher was its abundance, a trend that serves as a compelling signature of the ingestion of Earth-like rocky material. They calculated that each of the twins would have had to consume an additional 10–20 Earth masses of rocky material to produce the chemical signatures. Specifically, the star with the Jupiter-sized planet appears to have swallowed an extra 10 Earth masses while the star with the two Neptune-sized planets scarfed down an additional 20.
The results support the proposition that a star’s chemical composition and the nature of its planetary system are linked.
“Imagine that the star originally formed rocky planets like Earth. Furthermore, imagine that it also formed gas giant planets like Jupiter,” said Mack. “The rocky planets form in the region close to the star where it is hot, and the gas giants form in the outer part of the planetary system where it is cold. However, once the gas giants are fully formed, they begin to migrate inward, and as they do, their gravity begins to pull and tug on the inner rocky planets.
“With the right amount of pulling and tugging, a gas giant can easily force a rocky planet to plunge into the star. If enough rocky planets fall into the star, they will stamp it with a particular chemical signature that we can detect.”
Following this logic, it is unlikely that either of the binary twins possesses terrestrial planets. On one star, the two Neptune-sized planets are orbiting the star quite closely at one-third the distance between Earth and the Sun. On the other star, the trajectory of the Jupiter-sized planet grazes the star, taking it closer than the orbit of Mercury at the point of closest approach. The astronomers speculate that the reason the star with the two Neptune-sized planets ingested more terrestrial material than its twin was because the two planets were more efficient at pushing material into their star than the single Jupiter-sized planet was at pushing material into its star.
If the chemical signature of G-class stars that swallow rocky planets proves to be universal, “when we find stars with similar chemical signatures, we will be able to conclude that their planetary systems must be very different from our own and that they most likely lack inner rocky planets,” said Mack. “And when we find stars that lack these signatures, then they are good candidates for hosting planetary systems similar to our own.”
“This work reveals that the question of whether and how stars form planets is actually the wrong thing to ask,” said Stassun. “The real question seems to be: How many of the planets that a star makes avoid the fate of being eaten by their parent star?”