A team of Carnegie
investigated hydrogen liquefy in water from the Martian subsurface, and found
that Mars was formed from the same structure blocks as the Earth, and the
changes in the chemical composition of the planet began to occur in the course
of its subsequent evolution. This indicates that the terrestrial planets,
including Earth, the same source of water - chondritic meteorites. However,
unlike our planet, Mars rocks, which contain volatile components such as water,
can be processed deep in the bowels of the planet.
The researchers
examined two types of meteorites - one of them reflects the chemical
composition of the material from the surface of Mars, is in contact with the
atmosphere, while the other was a matter, having come out of a deep mantle of
the planet and little has changed with the structure. The analysis showed that
the sample from the surface contains about ten times more water than the sample
from the depths of Mars, which indicates the presence of the past a lot of
water on the surface of the red planet, scientists say.
The study was published
in the journal Earth and Planetary Science Letters.
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