Scientists have uncovered a possible hidden gem inside Mercury, the smallest planet in our photo voltaic system. Utilising information from Nasa’s MESSENGER spacecraft, researchers counsel that beneath Mercury‘s crust lies a diamond mantle roughly 10 miles thick.
Mercury has at all times been an enigma to scientists attributable to its distinctive traits, similar to its extraordinarily darkish floor, unusually dense core, and the early cessation of its volcanic exercise.One other puzzling function is the presence of graphite patches on Mercury’s floor, which led scientists to hypothesise that the planet as soon as had a carbon-rich magma ocean in its early historical past.
This ocean would have risen to the floor, creating the graphite patches and contributing to Mercury’s darkish look.
The identical course of that fashioned the graphite patches is believed to have additionally created a carbon-rich mantle beneath the floor. Nonetheless, the analysis staff proposes that this mantle is just not composed of graphene, as beforehand thought, however quite of diamond, one other allotrope of carbon.
“We calculate that, given the brand new estimate of the strain on the mantle-core boundary, and realizing that Mercury is a carbon-rich planet, the carbon-bearing mineral that might kind on the interface between mantle and core is diamond and never graphite,” defined staff member Olivier Namur, an affiliate professor at KU Leuven. “Our research makes use of geophysical information collected by the NASA MESSENGER spacecraft,” Namur added.
To analyze this speculation, the staff replicated the pressures and temperatures discovered inside Mercury’s inside utilizing a large-volume press right here on Earth. They subjected an artificial silicate, representing the fabric in Mercury’s mantle, to pressures exceeding seven gigapascals and temperatures as much as 3,950 levels Fahrenheit (2,177 levels Celsius). This allowed them to review how minerals much like these in Mercury’s early mantle would have reworked beneath these excessive situations.
The researchers additionally employed pc modelling to analyse information about Mercury’s inside, offering insights into the potential formation of the diamond mantle.
The invention of Mercury’s potential diamond mantle highlights the variations within the formation processes of the photo voltaic system’s rocky planets. “Mercury fashioned a lot nearer to the solar, seemingly from a carbon-rich cloud of mud. As a consequence, Mercury comprises much less oxygen and extra carbon than different planets, which led to the formation of a diamond layer,” Namur defined.
The researchers hope that this discovering could assist unravel different mysteries surrounding Mercury, such because the untimely finish of its volcanic section round 3.5 billion years in the past.
Wanting forward, the staff plans to analyze the thermal results of a diamond layer on the mantle/core boundary and eagerly awaits information from the BepiColombo mission, which can observe within the footsteps of MESSENGER and supply additional insights into Mercury’s inner construction and evolution.
Mercury has at all times been an enigma to scientists attributable to its distinctive traits, similar to its extraordinarily darkish floor, unusually dense core, and the early cessation of its volcanic exercise.One other puzzling function is the presence of graphite patches on Mercury’s floor, which led scientists to hypothesise that the planet as soon as had a carbon-rich magma ocean in its early historical past.
This ocean would have risen to the floor, creating the graphite patches and contributing to Mercury’s darkish look.
The identical course of that fashioned the graphite patches is believed to have additionally created a carbon-rich mantle beneath the floor. Nonetheless, the analysis staff proposes that this mantle is just not composed of graphene, as beforehand thought, however quite of diamond, one other allotrope of carbon.
“We calculate that, given the brand new estimate of the strain on the mantle-core boundary, and realizing that Mercury is a carbon-rich planet, the carbon-bearing mineral that might kind on the interface between mantle and core is diamond and never graphite,” defined staff member Olivier Namur, an affiliate professor at KU Leuven. “Our research makes use of geophysical information collected by the NASA MESSENGER spacecraft,” Namur added.
To analyze this speculation, the staff replicated the pressures and temperatures discovered inside Mercury’s inside utilizing a large-volume press right here on Earth. They subjected an artificial silicate, representing the fabric in Mercury’s mantle, to pressures exceeding seven gigapascals and temperatures as much as 3,950 levels Fahrenheit (2,177 levels Celsius). This allowed them to review how minerals much like these in Mercury’s early mantle would have reworked beneath these excessive situations.
The researchers additionally employed pc modelling to analyse information about Mercury’s inside, offering insights into the potential formation of the diamond mantle.
The invention of Mercury’s potential diamond mantle highlights the variations within the formation processes of the photo voltaic system’s rocky planets. “Mercury fashioned a lot nearer to the solar, seemingly from a carbon-rich cloud of mud. As a consequence, Mercury comprises much less oxygen and extra carbon than different planets, which led to the formation of a diamond layer,” Namur defined.
The researchers hope that this discovering could assist unravel different mysteries surrounding Mercury, such because the untimely finish of its volcanic section round 3.5 billion years in the past.
Wanting forward, the staff plans to analyze the thermal results of a diamond layer on the mantle/core boundary and eagerly awaits information from the BepiColombo mission, which can observe within the footsteps of MESSENGER and supply additional insights into Mercury’s inner construction and evolution.
