Young solar systems are chaotic. Our young Solar System was defined by cascading collision. Some of the chaos can be traced back to asteroids that crashed into Earth.

Since their formation billions of years ago, asteroids have remained essentially unchanged. Because differentiated asteroids have mantles that protect their interiors from space weathering, they're like rocky time capsule.

Not all asteroids were still intact. The mantles were stripped away from the iron core and then shattered. Pieces fell to the ground. King Tut was buried with a dagger made from an iron meteorite, and Inuit people made tools out of iron meteorites for hundreds of years.

Iron meteorites have information that scientists are interested in. The study looked at the amount of metal in iron meteorites. The authors were able to more tightly control the timing of some events in the early Solar System by measuring the amount of those isotopes.

The paper was published in Nature Astronomy. Alison Hunt is from the National Centre of Competence in Research.

Since their formation billions of years ago, asteroids in the solar system have remained relatively unchanged. The conditions of the early solar system are preserved in these archives.

The ancient Egyptians and the Inuit had no idea about decay chains. We know how long it takes for some elements to decay into others. The short-lived107Pd–107Ag decay system is at the center of this work. The chain is used to detect nuclides from the early Solar System.

The iron meteorites that were collected were once part of the iron core of asteroids. They used a mass spectrometer to measure the concentrations of different elements after isolating them. This research is dependent on a specific element of Silver.

One of the iron meteorites that the researchers analyzed in their study. Image Credit: Aurelia Meister
One of the iron meteorites that the researchers analyzed in their study. Image Credit: Aurelia Meister

The metallic cores in asteroids were heated during the first million years of the solar system. There was an isotope of Silver in the cores as they cooled. The researchers were able to determine how quickly the asteroid cores cooled.

Researchers have studied asteroids in this way before. The effects of GCRs on the ratios were not accounted for in previous studies. The amount of 107 Ag and109 Ag can be decreased by disrupting the neutron capture process. The new results are also counted for G CR interference.

We were able to correct the Silver isotope measurement for distortions caused by the irradiation of the samples. We were able to date the collision more precisely than before. After the formation of the solar system, all the asteroidal cores we examined had been exposed at the same time.

An artist's conception of an asteroid collision in the belt between Mars and Jupiter. Credit: NASA/JPL-Caltech
An artist’s conception of an asteroid collision in the belt between Mars and Jupiter. Credit: NASA/JPL-Caltech

Four million years is not long in astronomy. All of the asteroids that were measured had their core exposed, meaning they were stripped of their mantles. The cores all cooled off at the same time. The studies showed that the cooling was rapid, but they couldn't say how long it would take.

The Solar System had to be very chaotic in order for the asteroids to have the ratios they did.

Hunt says that everything seemed to have been smashing together. She wants to know why.

There is a period of chaotic crashes. According to the paper, there are at least two possibilities.

The solar system has giant planets. If they were unstable at that time, they could have rearranged the inner Solar System, disrupted small bodies, and triggered a period of increased collision. The Nice model is where this scenario is located.

Gas drag is a possibility.

Artist’s impression of the Solar Nebula. Image credit: NASA

The Sun was surrounded by a cloud of gas and dust when it was a young star. The planets would eventually form there as well as the asteroids. The disk changed over time in the Solar System.

The density of the gas slowed down the motion of asteroids and planetesimals. The Sun produced more wind and radiation as it went on. The solar wind and radiation dissipated the solar nebula. There was less drag on objects as it dissipated. asteroids accelerated and collided with each other more frequently without the effect of dense gas.

This figure from the study shows the evolution of differentiated iron meteorite bodies in the early Solar System. At the top, the parent bodies accrete and differentiate within the first ~3 Myr after CAI formation. Then there are two competing scenarios for the period of increased collisions among asteroids. Scenario A is the gas dissipation scenario, and the one that the research team thinks fits the data best. Scenario B is the Nice model, where a giant planet creates instability and causes the period of increased collisions. Image Credit: Hunt et al. 2022.
This figure from the study shows the evolution of differentiated iron meteorite bodies in the early Solar System. At the top, the parent bodies accrete and differentiate within the first ~3 Myr after CAI formation. Then there are two competing scenarios for the period of increased collisions among asteroids. Scenario A is the gas dissipation scenario and the one that the research team thinks fits the data best. Scenario B is the Nice model, where a giant planet creates instability and causes a period of increased collisions. Image Credit: Hunt et al. 2022.

The reduction of gas drag is to blame according to Hunt and her colleagues.

Maria Schnbchler explained that the theory that best explained the energetic early phase of the solar system indicated that it was caused by the solar nebula. The Sun was born out of a cloud of gas that was left over from another planet. It was blown away by the sun's rays for a few million years.

Improvements in laboratory measurement techniques allow us to infer important processes that took place in the early solar system, like the likely time by which the solar nebula had gone. The world was still in the process of being born. Ultimately, this can help us to better understand how our own planets were born, but also give us insights into other planets.

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