ECLAIR+TONNERRE+PLUIE=UNE SEULE OPERATION.pdf


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English: LIGHTNING + THUNDER + RAIN = ONE OPERATION
1-Photolysis: (dissociation or photolysis) of ocean water is in the decomposition of the water molecule into hydrogen molecules (H2) and
carbon (O) under the effect of solar radiation, the occurrence ultraviolet.
https://fr.wikipedia.org/wiki/Photolyse
www.google.dz/search?q=photolyse

http://www.u-helmich.de/bio/lexikon/P/photolyse-wasser.html
Due to the decrease in ozone in some regions of the globe, sunlight
reaches the surface of the earth and enriched with UV-C radiation (λ = 100
-280 nm) of short wavelength (Lloyd, 1993), between 11 and 16 h their
Due to the decrease in ozone in some regions of the globe, sunlight reaches the
intensity
still
high
and
furtherwith
towards
14 pm, the
smaller
surface of is
the
earth
and
enriched
UV-C radiation
(λ =UV
100through
-280 nm)aof
short
distance
in (Lloyd,
the atmosphere
and are
not16
intercepted
by the
ozone
wavelength
1993), between
11 and
h their intensity
is still
high and
molecules,
they14manage
surface
of thedistance
earth and
dissociate
water
further towards
pm, the to
UVthe
through
a smaller
in the
atmosphere
and
molecules
H2 and by
O free,
their molecules,
rate is higher
the mountains
and of
are
are
not intercepted
the ozone
theyin
manage
to the surface
the
earth
and dissociate
water
molecules
H2 and O free, their rate is higher in the
reverberated
through
water
and snow.
mountains
and
are
reverberated
through
water and snow.
http://biologiedelapeau.fr/spip.php?mot162
Oxygen escapes

http://biologiedelapeau.fr/spip.php?mot162

For an O-H bond is broken, it is necessary to provide an energy at least equal to the DOH binding energy is 461.6 kJ mol-1,
The energy for a photon to break the O-H bond:

UV-A (λ = 320–400 nm),
UV-B (λ = 280–320 nm),
UV-C (λ = 100–280 nm)
http://acces.ens-lyon.fr/acces/terre/eau/comprendre/proprietes-physico-chimique-de-leau
2- Where will the H2 molecules and O atoms?
Both lighter than air (air = 29/29 = 1, H2 = 2/29 = 0.06 and O = 16/29 = 0.55), They will be driven by currents of warm air upward, lightest
go up more and form what is called the positive charges (2H⁺), the second rise unless it is positioned below and form what is called the
negative charges (Oˉ ˉ), is due to their ionization:
- The opposition of two mechanical forces (those currents of warm air upward and downdrafts of cold air from which compression and
friction) on the one hand and
-the action of sunlight on the gas (ionization since they are closer to the sun as it rises)
2 gas at a favourable compression ratio combine in an explosive chemical reaction (synthesis of water is explosive), they form water
(rainfall) and everything is explained as if by magic (in an explosion was what the spark of lightning, the sound of the explosion thunder
and what the result of this explosive reaction is water).

2H⁺ + 2 ésynthesis

½ O2 + (2H⁺) + 2é

1-You will notice quickly that what we call positive charges are always
placed at the top, they are in fact the hydrogen released by photolysis of
ocean waters and other (action of UV) and thus the lighter will rise most
with respect to oxygen (it supports more cold than oxygen, it liquefy
only -250 ° C)
2-You still notice what is called negative charges are always placed
below the first, they are in fact only the oxygen released him also
photolysis of ocean waters and other (action of UV) and thus heavier as
hydrogen (supports less cold than hydrogen, it liquefies at -196 ° C)
3-The light of the flash reaches us first (299,792,458 m / s), the sound of
the explosion was thunder (340 m / s) in second and finally raindrops
which fall speed is less than those of the light and sound

It occurs in 24 hours around the earth between 2.000 to 5.000 storms per second:
http://www.planetoscope.com/atmosphere/252-nombre-d-orages-dans-le-monde.html
Every storm cell can produce more than 100 flashes per minute:
http://www.astrosurf.com/luxorion/meteo-orages3-eclairs.htm
This means that form the rainwater between 200.000 to 500.000 per second Once in the atmosphere by chemical reaction (synthesis),
then coalescing once formed the cloud but the initial origin of his birth remains (H2 + ½ O2  H2O + heat).