Physical model explains the origin of Earth’s water
Equipped with Newton’s law of universal gravitation (published in Principia 330 years ago) and powerful computational resources (used to apply the law to more than 10,000 interacting bodies), a young Brazilian researcher and his former postdoctoral supervisor have just proposed a new physical model to explain the origin of water on Earth and the other Earth-like objects in the Solar System.
The article, “Origin of water in the inner Solar System: Planetesimals scattered inward during Jupiter and Saturn’s rapid gas accretion”, was published in the planetary science journal Icarus.
The authors of the article are André Izidoro, who is affiliated with São Paulo State University’s Guaratinguetá School of Engineering (FEG-UNESP) and supported by a Young Investigator Grant from FAPESP, and the American astrophysicist Sean Raymond, who is currently with the Bordeaux Astrophysics Laboratory in France.
“The idea that Earth’s water came predominantly from asteroids isn’t new. It’s practically a consensus among researchers. Our work isn’t groundbreaking in that sense. What we did was associate the asteroid contribution with the formation of Jupiter. Based on the resulting model, we ‘delivered to Earth’ amounts of water consistent with currently estimated values,” Izidoro told Agência FAPESP.
Estimates of the amount of water on Earth vary a great deal. If the unit of measurement is terrestrial oceans, some scientists speak of three to four of them, while others estimate dozens. The variation derives from the fact that the amounts of water in the planet’s hot mantle and its rocky crust are unknown. In any event, the model proposed covers the full range of estimates.
“First of all, it’s important to leave aside the idea that Earth received all its water via the impacts of comets from very distant regions. These ‘deliveries’ also occurred, but their contributions came later and were far less significant in percentage terms,” Izidoro said. “Most of our water came to the region currently occupied by Earth’s orbit before the planet was formed.”
To understand how this happened, it is worth restating the scenario defined in the conventional model of the Solar System’s formation and then adding the new model for the advent of water.
The initial condition is a gigantic cloud of gas and cosmic dust. Owing to some kind of gravitational disturbance or local turbulence, the cloud collapses and is attracted by a specific inner region that becomes a center.
With the accumulation of matter, at about 4.5 billion years ago, the center became so massive and hot that it began the process of nuclear fusion, which transformed it into a star. Meanwhile, the remaining cloud continued to orbit the center and its matter agglutinated to form a disk, which later fragmented to define protoplanetary niches.
“The water-rich region of this disk is estimated to have been located several astronomical units from our Sun. In the inner region, closer to the star, the temperature was too high for water to accumulate except, perhaps, in very small amounts in the form of vapor,” Izidoro said.
An astronomical unit (AU) is the average distance from the Earth to the Sun. The region between 1.8 AU and 3.2 AU is currently occupied by the Asteroid Belt, with hundreds of thousands of objects.
The asteroids located between 1.8 AU and 2.5 AU are mostly water-poor, whereas those located beyond 2.5 AU are water-rich. The process whereby Jupiter was formed can explain the origin of this division, according to Izidoro.
“The time elapsed between the Sun’s formation and the complete dissipation of the gas disk was quite short on the cosmogonic scale: from only 5 million to, at most, 10 million years,” he said.
“The formations of gas giants as massive as Jupiter and Saturn can only have occurred during this youthful phase of the Solar System, so it was during this phase that Jupiter’s rapid growth gravitationally disturbed thousands of water-rich planetesimals, dislodging them from their original orbits.”
Jupiter is believed to have a solid core with a mass equivalent to several times that of Earth. This core is surrounded by a thick and massive layer of gas. Jupiter could only have acquired this wrapping during the solar nebular phase, when the system was forming and a huge amount of gaseous material was available.
The acquisition of this gas by gravitational attraction was very fast because of the great mass of Jupiter’s embryo. In the vicinity of the formation of the giant planet, located beyond the “snow line”, thousands of planetesimals (rocky bodies similar to asteroids) orbited the center of the disk and, simultaneously, attracted each other.
The rapid increase of Jupiter’s mass undermined the fragile gravitational equilibrium of this system with many bodies. Several planetesimals were engulfed by proto-Jupiter. Others were propelled to the outskirts of the Solar System.
In addition, a smaller number were hurled into the disk’s inner region, delivering water to the material that later formed the terrestrial planets and the Asteroid Belt.
“The period during which the Earth was formed is dated to between 30 million and 150 million years after the Sun’s formation,” Izidoro said. “When this happened, the region of the disk in which our planet was formed already contained large amounts of water, delivered by the planetesimals scattered by Jupiter and also by Saturn."
"A small proportion of Earth’s water may have arrived later via collisions with comets and asteroids. An even smaller proportion may have been formed locally through endogenous physicochemical processes. But most of it came with the planetesimals.”
His argument is supported by the model he built with his former supervisor. “We used supercomputers to simulate the gravitational interactions among multiple bodies by means of numerical integrators in Fortran,” he explained.