The atmosphere of the
planet
The planet's atmosphere has been evolving since detachment from the
parent star, determined by the interactions of the vector properties of
energy.
The atmosphere of the young planet continues the interactions of the
atmosphere from which it was formed. Thus, initially fed with the hydrogen
of the
mother star, it develops the orthogonal vector circuits (magnetism and
electricity).
Centroidal pressure rises relatively quickly, multiplying hydrogen.
The increase in kinetic energy determines the phenomenon what satellites
reproduction. After the end of the reproduction, with the diminished kinetic
energy, the hydrogen boiling begins to generate the atoms of the elements
by "bud".
The atmosphere is enriched with helium atoms, as seen in the atmosphere
of
the star and continues with heavier elements, which settle to form the
crust
of the planet. The reactions of hydrogen becomes a real laboratory for
the
formation of elements, volcanoes and mountains. In the atmosphere, hydrogen
is gradually replaced by heavier gases, carbon compounds as seen on Venus,
and then nitrogen and oxygen as it exists on Earth. Hydrogen compounds
with carbon are deposited in the form of hydrocarbon deposits, and those
with oxygen form seas and oceans. On Earth, the consolidation of the solid
crust lasted a long time, during which the moon lost its kinetic and potential
energy, becoming a solid sphere, the former electrode leaving a empty
place,
a cavity with a radius of about one-third the radius of the sphere.
This was the period of the planet's youth.
The maturity period of the planet.
Under the conditions of adequate temperatures and circadian rhythm, the
vector properties of solid, liquid and gaseous media organize a multitude
of
structures with vector oscillators, more or less ephemeral. The simplest
ephemeral structures are known as viruses. It follows that from structures
with vector oscillators, only environmentally compatible structures remain
perennial. The structures of viruses being sometimes incompatible with
the
environment, appear and disappear seasonally. The vector properties of
the
energy in the structure of the virus continue to organize these structures.
The selected structure is euglena viridis, which develops in the liquid
medium
and then migrates to the solid and gaseous medium. Thus begins the
expansion of the biosphere, through the continuous development of the
vegetable kingdom and the animal kingdom. Two steps, the Proterozoic and
Phanerozoic eons, intervened in the development of the biosphere, by
diminutions the solar radiation at the formation of the planets Venus
and
Mercury. In the evolution of the planet, the biosphere began with viruses,
develops and ends with viruses. Viruses are one of the natural factors
in the
selection of structures, along with climatic factors, on which viruses
also depend.
Of all the animal species in the biosphere, the human species has been
shown to be the devastating species of the biosphere, of its own living
conditions, with the aim of ... improving the conditions of life, The
human
species knows no bounds in the actions of destroying the biosphere. The
human
species is the only species that fights against natural selection. Remedial
measures taken as a result of the destruction of the biosphere prove to
be useless.